Fugro Airborne Surveys BASIC EM INTERPRETATION REPORT and … · 2017. 1. 16. · 4 I Introduction Between November 13 th 2007 to December 18 2007 and January 11 th 2008 to February

Fugro Airborne Surveys

BASIC EM INTERPRETATION REPORT

Airborne Magnetic

and HeliGEOTEM II Survey

ADELAIDE, BAY, KING, AND YORK PROPERTIES, ONTARIO

Job No. 07309 MacDonald Mines Exploration Ltd.

Fugro Airborne Surveys

BASIC EM INTERPRETATION REPORT AIRBORNE MAGNETIC AND HELIGEOTEM II SURVEY ADELAIDE, BAY, KING, AND YORK PROPERTIES ONTARIO JOB NO. 07309

Client: MacDonald Mines Exploration Ltd. 1000 - 141 Adelaide Street West Toronto, Ontario M5H 3L5 Date of Report: July 2008

3

TABLE OF CONTENTS

INTRODUCTION 4

SURVEY OPERATIONS 5

Location of the Survey Area 5

INTERPRETATION 6

General Magnetic Theory 6

Magnetic Interpretation Procedures 6

Overview of the Magnetic Field 7

Overview of the Electromagnetic Field 8 Apparent Conductance 8

Electromagnetic Interpretation Procedures 10

Conductors in the Survey Areas 11 Adelaide Block 12 Bay Block 12 King Block 14 York Block 15

APPENDIX A - EMQ MODELING RESULTS 16

APPENDIX B – EM ANOMALY LISTING 43

4

I Introduction

Between November 13th 2007 to December 18th 2007 and January 11th 2008 to February 4th 2008, Fugro Airborne Surveys conducted a HeliGEOTEM® II electromagnetic and magnetic survey of the Adelaide, King, Bay, and York Properties on behalf of MacDonald Mines Exploration Ltd. Using Webequie, Ontario as the base of operations 6,344 line kilometres of data were collected using two survey systems carried by an AS-350 B2 Helicopter and an AS-350 B3 Helicopter (similar to helicopter shown in Figure 1). The interpretation is presented in colour on paper and GEOSOFT digital map files. A complete processing report is presented as a separate document. Refer to the processing report for more details on the survey and system specifications as well as information on the data processing and final products. The following appendices to the processing report are of particular interest to the interpretation:

� Helicopter Airborne Electromagnetic systems. � Airborne Transient EM Interpretation. � Multi-component modeling. � The Usefulness of Multi-component Time-Domain Airborne EM Measurement.

Figure 1: AS-350 B2 Helicopter similar to that used by Fugro Airborne Surveys.

5

II Survey Operations

Location of the Survey Area The Adelaide, King, Bay, and York Properties (Figure 2) were flown with Webequie, Ontario as the base of operations. A total of 657 lines were flown with a spacing of 100 m between lines, and a spacing of 1000 m between tie-lines totalling 6,344 km for the complete survey.

Figure 2: Location of the Survey Area.

6

III INTERPRETATION

General Magnetic Theory The Earth's magnetic field, which changes from over 60,000 gammas in a vertical direction at the poles to about 30,000 gammas in a horizontal direction at the equator, induces a secondary magnetic field in rock bodies containing ferromagnetic minerals. It is this property to become magnetized by an external field that is described as the susceptibility of a rock. Some rocks contain a natural or thermoremanent magnetization that was acquired when the rock was last heated above the Curie point and subsequently cooled. The direction of this remanent magnetization is parallel to the magnetic field that prevailed during the cooling period. These fields, both the induced and remanent, disturb the otherwise smooth magnetic pattern of the Earth's field, and it is these perturbations that are of prime interest in aeromagnetic interpretation. The crystalline rocks of igneous or high-grade metamorphic origin, such as granite, basalt, gneiss and schist, usually contain sufficient quantities of ferromagnetic minerals (mainly magnetite) that their influence on the earth's field can be observed even when covered by sedimentary sections thousands of feet thick. The magnetic pattern over large areas of a single rock type is generally consistent throughout, and whenever the magnetic character changes, it usually implies a change in the rock composition. For example, the contact between a granitic mass and an ultrabasic unit can usually be precisely positioned where the magnetic pattern begins to change from the usual quiet character of granite to the more disturbed pattern of an ultrabasic rock body. The study of magnetic anomalies does, to some degree, depend upon the latitude; in high latitudes attention is devoted to positive anomalies, while at the equator negative anomalies are of prime interest. This is due to the inclination of the earth's magnetic field, which is near vertical, 90°, at the poles, horizontal, 0°, at the equator, and about 77 ° north in this survey area. In such a steep magnetic inclination, the strike of a magnetic body has little effect upon the magnitude and symmetry of the anomaly it produces. An E-W dyke will be primarily positive, with a very weak negative on its north side. The same dyke striking magnetic north (azimuth 353 in this area) will be a symmetrical positive, but only about 95% of its E-W amplitude.

Magnetic Interpretation Procedures In the basic electromagnetic interpretation, magnetic features in the vicinity of conductive targets are studied with regard to shape, size, strike and grouping to aid the evaluation of conductors and their potential correlation with basement. Basement lineaments relating to EM conductors are shown on the interpretation maps.

7

Overview of the Magnetic Field The survey areas lie in a magnetically active area in the vicinity of the “ring of fire” in the James Bay lowlands. Most of the strong magnetic features lying around the survey areas are generated by mafic to intermediate metavolcanics1 and Archean ultramafics.

1 All references to geology and discoveries from: Ring of Fire, McFauld’s Lake Area Geology Map, Noront Resources Ltd., UC Resources Ltd., Spider Resources Inc., and KWG Resources Inc. December 2007. Scale 1:125000.

The survey areas with the regional magnetic field.

8

Overview of the Electromagnetic Field Optimal products for the areas were selected and generated from the EM data, these products are: Adelaide Bay • EM Anomalies • EM Anomalies • Apparent Conductivity dB/dt Z channel 7 • Apparent Conductivity dB/dt Z channel 7 • Apparent Conductivity B-field Z channel 6 • Apparent Conductivity B-field Z channel 15

King York • EM Anomalies • Apparent Conductivity dB/dt Z channel 7 • Apparent Conductivity dB/dt Z channel 6 • Apparent Conductivity B-field Z channel 8

Apparent Conductance

The apparent conductivity was calculated by fitting channel specified channel of the dB/dt or B Field Z-coil response to the homogeneous-half-space model. Prior to the fitting, the data is deconvolved to the step response in order to provide a linear relationship as the conductivity of the ground increases from the resistive limit to the inductive limit. The apparent conductivity provides the maximum information on the near-surface conductivity of the ground which, when combined with the magnetic signature, provides good geological mapping.

9

Electromagnetic Anomaly Selection Traditionally with fixed-wing, towed-bird TDEM systems, such as GEOTEM and MEGATEM, the EM anomaly selection is done using the response from the X-coil data by fitting the peak amplitudes of the anomalies to a set of nomogram curves based on the vertical plate model. This allows for the determination of depth and conductivity-thickness-product (CTP) of the conductor (assuming, of course, that the vertical plate model is a valid representation of the conductive source). This is made possible by the fact that, due to the geometry of the fixed-wing, towed-bird systems, the peak of the X-coil response will correspond to the axis of a vertical plate-like conductor. However, with the HeliGEOTEM response, because of the difference in the Tx – Rx geometry, neither the response from the X or Z coil will peak over the axis of the conductor. Instead, over a vertical conductor, the response will show a cross-over on the X-coil and a minima on the Z-coil. Because of this, the anomaly peaks with the HeliGEOTEM data cannot be used to fit to the reference nomogram to derive CTP and depth-to-source. The EM anomaly map provided and used for the interpretation is instead an anomaly trend map which simply shows the locations of the anomaly peaks from the Z-coil response (from either the dB/dt or B-Field response) with an indication of the number of channels deflected. There is no fitting to a nomogram allowing for the calculation of CTP and depth-to-source. In the EM anomaly listing, provided as an appendix to this report, the UTM coordinates given correspond to the locations of the anomaly peaks but not the conductor axis. As part of the interpretation, where an anomaly response is judged to represent a vertical conductor, the assumed position of the conductor axis is shown on the map by the axis that is drawn. In the profile example below, showing HeliGEOTEM responses measured over vertical conductors, the locations of the EM anomalies shown on the map and the corresponding UTM coordinates given in the anomaly listing would correspond to the positions marked by a P. The interpreted position of the conductor axes are shown at the locations marked A.

10

Where the anomaly is suitably well defined and not overly disturbed by the presence of other closely spaced conductors, the EM response can be modeled interactively using a routine called EMQ which provides information on the position of the conductor, its depth below surface, its strike and dip as well as the conductivity of the source. Refer to Appendix A.

Electromagnetic Interpretation Procedures The general approach to EM interpretation is two-fold. One is to work from the data in plan form (maps), correlating back to the data in profile form; the other is to work from the profiles back to the maps. The basis of target selection is to look for "anomalous" responses. Some of these will stand out on the maps as somewhat isolated features along (hopefully) favourable structural intercepts. Conversely, some localized changes in conductivity may only be apparent in profile form and may not stand out on the maps due to surrounding conductivity. So, a general review of the EM anomalies in profile form is done to search for well-defined symmetrical shape, moderate amplitude, slow decay, etc., then checked on the maps for strike length, structural (magnetic/geologic) support and overall conductivity pattern. The conductor axes and zones were compared with the magnetic signature to separate the basement conductors from those arising from overburden. The magnetic signature over a shield area arises almost exclusively from the crystalline basement. Two levels of correlation with magnetic/geologic basement were noted: - structurally favorable (along contacts, intersected by faults, near intrusives, etc.); - coincidence of EM and magnetic bodies of similar dimensions. At the end of this process, the EM selections will normally fall into six groups, which will be: Based on the EM signature A. Anomalous on the maps and having good anomaly characteristics in profile form; B. Non-distinct on the maps but having good anomaly characteristics in profile form;

C. Anomalous on the maps but lacking good anomaly characteristics in profile form; Based on the Magnetic signature

1. With a magnetic coincidence suggesting a common source; 2. Showing evidence of structural control from the magnetic signature; 3. Showing no support from the magnetic signature. These six groups will then be recombined into nine categories, ordered in terms of their potential as massive sulphide or mineral targets, A-1 having the greatest potential to C-3 having the least potential.

Categories: A-1, A-2, A-3, B-1, B-2, B-3, C-1, C-2 and C-3 The EM responses discussed in the following section identify those anomalies, which generally met the criteria associated with possible mineralization. The category assigned to each selection is based on the criteria outlined above which can be summarized by the table below:

11

CLASSIFICATION OF EM SELECTIONS

CATERGORY

Response in plan View (from maps)

Profile expression

Magnetic signature

A-1 Anomalous Good Coincident anomaly A-2 Anomalous Good Structural support A-3 Anomalous Good No support B-1 Non-distinct Good Coincident anomaly B-2 Non-distinct Good Structural support B-3 Non-distinct Good No support C-1 Anomalous Poor Coincident anomaly C-2 Anomalous Poor Structural support C-3 Anomalous Poor No support

As some of the conductor axes are quite extensive, often crossing many survey lines, classification will be done on a selection of anomalies that represent the highest priority points of the bodies, instead of classifying each anomaly on every line separately which may at times be redundant. Conductors listed that do not have a classification assigned are generally bodies that display poor plan view response and profile expression and therefore do not fit into the A, B or C groups. However, these conductors do display evidence of weakly conductive properties and are included in the conductor list. A reminder that category A-1 identifies the greatest potential for mineralization with the priority dropping to category C-3 having the least potential. Refer also to Appendix B of the Logistics and Processing Report (Airborne Transient EM Interpretation), which provides more general information on the interpretation of time-domain electromagnetic data.

Conductors in the Survey Areas Significant conductors within the survey areas have been outlined on the interpretation map and are described below. The conductors are classified as conductive zones, points and axes. An axis describes a conductor that displays a relatively narrow, linear feature with defined profile response, often with indication of vertical extent. Single point anomalies are generally notable responses seen only on one line, and depending on their strength and the survey line spacing, can often be considered good exploration targets. Areas interpreted as conductive zones are generally broad conductors displaying a well-defined boundary on at least one of the EM grids, in this case the apparent conductivity and channel amplitude grids. Potential faults and basement lineaments are shown on the interpretation map in the vicinity of the conductors described below. Due to the abundance of strong magnetic response, the first vertical derivative grid is displayed as the base grid in order to help show the extent of the magnetic/electromagnetic correlation.

12

Adelaide Block

Target Line Range

Best response(s)- Line/Anomaly

Observations Category

1 40050-40080 40060/B

• Low amplitude, east-west trending axis with a weak profile response and poor map response.

• Poor magnetic correlation, although does lie along a break in some weak magnetic trends.

B-2

2 40060 40060/A • Single point EM anomaly, weak profile response and poor map

response. • No noted magnetic correlation.

B-3

3 40270-40320 40300/B

• Weak to moderate strength EM axis. Categorized as a weak A-2 target as the profiles suggest vertical extent and the map response is relatively good for this block.

• Good magnetic correlation, lying partially along a weak gradient and immediately south of a slightly stronger gradient.

A-2

4 40770-40870 40800/A

• Moderate strength, east-west trending conductor axis. • EMQ modeling done on lines 40790 and 40800 suggesting a near

vertical body, or a body steeply dipping to the south. • Good magnetic correlation, lying along several well-defined gradients.

A-1

5 40670-40700

40690/A

• Isolated, short strike, moderate strength axis. • EMQ modeling done on lines 40680 and 40690, suggesting the body

dips to the north. • Good magnetic correlation.

A-2

6 40790-40860 - • Weak surficial response -



Bay Block

Target Line Range



1 60400-60500 60430/A

• Moderate strength to strong conductor. • EMQ modeling done on lines 60420 and 60470 suggest a roughly flat

lying body. • Good correlation with a magnetic body of similar size and shape.

A-1

2 60430-60470

60450/A

• Strong, short strike, isolated conductor with an excellent B-field response.

• This is the Eagle 1 discovery. • EMQ modeling done on line 60450 suggesting a shallow dipping body,

although modeling results are moderate at best. • Excellent correlation with short strike magnetic response or similar size

and shape. Lies along a known fault.

A-1

3 60520-60580 60560/A

• Weak, low amplitude EM response. Could represent a near surface, flat lying or tabular body, or possibly a response from a deep conductor.

• Body lies on the flank of a strong magnetic response. • No notable correlation with topography.

C-1

13

Target Line Range



4 60640-60690

60670/A

• Weak, low amplitude EM response. Could represent a near surface, flat lying or tabular body, or possibly a response from a deep conductor.

• Body lies on the flank of a strong magnetic response. • No notable correlation with topography.

C-2

5 60700-60720 60710/A

• Moderate strength, sort strike conductor axis. • Excellent correlation with the magnetic field data, lying coincident with a

“bulge” in the vertical gradient, along a strong, extensive magnetic body. A-1

6 60780-60810 60790/A

• Moderate strength, sort strike conductor axis. • Excellent correlation with the magnetic field data, lying coincident with

the strongest section of an extensive magnetic body A-1

7 60820-60900

60870/A

• Short strike conductor axis dipping to the north. This body is likely related to conductor zone 9 to the northeast as it lies along the same magnetic trend.

• This target and target 8 below lie in the vicinity of the Freewest/Spider/KWG chrome and PGM discovery.

• Excellent correlation with the magnetic field data.

A-1

8 60860-60940 60920/B

• Well-defined conductor axis spanning about 9 survey lines, or about 1 km. Profile shapes and EMQ modeling indicate a north dipping body.

• This target and target 7 above lie in the vicinity of the Freewest/Spider/KWG chrome and PGM discovery.

• This conductor lies along a weak magnetic trend.

A-2

9 60890-61060

60950/A

• Strong, flat-lying or tabular body. Possibly related to conductor 7 located to the southwest along the same magnetic trend, although appears to lie in a different orientation.

• EMQ modeling done on line 60960 using the sphere model. • Excellent correlation with the magnetic field data.

A-1

10 61050-61110 61080/C

• Well-defined, short strike EM axis. • EMQ modeling done on lines 61070 and 61080 suggesting a near

vertical body. • Excellent correlation with a short section of a magnetic body adjacent to

a more extensive body.

A-1

11 60940-61320

60980/A 61060/A 61300/D

• Very extensive EM axis with several sections with different characteristics. The strongest response is along a ENE trending section from lines 60940-61120. Five EMQ modeling points were done along this section, all suggesting a near vertical body. Excellent correlation with a narrow magnetic body.

• A weaker section of the axis is located from lines 61130-61180 where the trend of the body shifts to a NE trend. The weaker section lies at a potential fault where weathering/alteration may have weakened the conductive source.

• A third moderate strength section lies on a NE trend terminating at a potential fault at around line 61330. Excellent correlation with a weaker magnetic body as seen with the section of the axis to the southwest.

• The UC/Spider/KWG McFauld’s Lake VMS discovery #7 lies at around line 61210/61220.

• A short strike body lies immediately north of the axis on lines 61100-61130, these bodies are likely related.

A-1

12 61260-60370 61290/D

• A weak to moderate strength body lying on a ENE trend. • Excellent correlation to a magnetic body of similar size which lies

adjacent to a magnetic body of greater extent. • West end of the axis terminates at a potential fault.

A-1

14

Target Line Range



13 61230-61350

61340/B

• Short strike axis trending in a NE direction which appears to be controlled by several potential faults identified by the magnetic field data.

• EMQ modeling done on lines 61320-61340 show a north-west dipping structure.

• Excellent correlation with an extensive magnetic body. • Axis lies along a small riverbed, but not parallel to the river.

A-1

14 61350-61390

61360/C

• Short strike axis trending in a NE direction which appears to be controlled by several potential faults identified by the magnetic field data. This axis is likely related to axis 11 as it lies along the same magnetic body.

• EMQ modeling done on lines 61360-61370 show a north-west dipping structure.

• Excellent correlation with an extensive magnetic body. • This body likely extends outside of the survey area to the northeast

A-1

15 61230-61360 61350/A

• A weak-moderate strength axis lying just to the north of axes 13 and 14. • Profile shape suggest a flat lying or tabular body. • This axis lies between two strong magnetic bodies but appears to trend

about 30° off strike from the trend of the magnetic features. • Axis lies along a small riverbed, but not parallel to the river.

A-2

16 61650-62300 -

• Broad, near surface response. Several areas of higher amplitude response shown in solid hatching, probably of no exploration significance.

-

17 60060-61470 -

• Broad, near surface response. Several areas of higher amplitude response shown in solid hatching, probably of no exploration significance.

-

King Block

Target Line Range



1 51110-51200

-

• Weak, low-amplitude conductor axis. Although weak, the profile shapes suggest a near vertical conductor. Peak to peak distance suggests the body lies at approximately 275 metres.

• Correlation with a weak magnetic trend is noted. No correlation with the topography

-

2 51070-51200 -

• Broad, moderate strength near-surface response. Likely a result of near surface alteration.

• No noted correlation with the magnetic field data or topography -

3 50240-50640 - • Weak, surficial response associated with drainage patterns.

• No magnetic correlation -

4 50180-50240 - • Weak, surficial response -

5 50170-50240 - • Weak, surficial response -

6 50010-50080 - • Weak, surficial response

• Weak correlation to a magnetic trend and a potential fault -

7 50010-50110 - • Weak, surficial response

• Weak correlation to a magnetic trend and a potential fault -

15

York Block

No conductors have been identified in the York block. No interpretation or anomaly map has been generated. We trust this data will further your exploration program; and we remain available for questions and any feedback that you are able to provide. Respectfully Submitted: Michael J. Cain, P. Eng.

16

Appendix A - EMQ Modeling Results

The modeling with EMQ is done from the “Moment” data, which is itself calculated from the B-Field response. As such, weaker conductors which have a short time constant and a poorer B-Field response will generally not provide a sufficiently good signature on the derived Moment response to allow reliable modeling of the anomalies. Also, in order to be able to fit a response with a reasonable degree of confidence, the anomaly itself must be well defined with a minimum of disturbance from neighboring conductors. This means that, in order to be able to able to model an anomaly successfully, it must be a singular response and relatively isolated. A strong response, which is part of a cluster of anomalies, may not provide reliable modeling results if is too disturbed by the effect of nearby conductors. Notes on the EMQ presentation:

• The BLUE profile trace represents the measured response. • The RED profile trace represents the model results • The cross-section window shows a “sphere” which is the default model used by the

application. However, in this case, the simulated “plate” response was used to better reflect the linear – elongated nature of the responses. This is done by channeling all the current flow along one plane of the sphere, thus simulating the response from a plate. The outline of the plate corresponds to the plane drawn through the sphere.

• In the profile windows, the right-hand side of the image always corresponds to either North or East.

• The three profile widows, Top, Middle and Bottom, correspond to the response from the X, Y and Z coil respectively, or when modeling different moments from the same component would correspond to the 2nd, 3rd and 4th moment of the Z coil for example.

• EMQ solves for the following parameters: Position, depth, conductivity, dip, strike and diameter. When using the simulated “plate” response, the value of the “diameter” is a reflection of the total surface area of the conductor and is not an indication of the width of the conductor.

• If an “offset” is noted, this is relative to the flight line. However, the position given is correct and reflects the offset.

General comments about the modeling: As is the case for all modeling, the better the fit, the more confident the results. Although the “sphere” model is the fundamental model used by the program, the simulated” plate response is more commonly used to best approximate the conductors. Looking closely at the differences between the measured and modeled profiles, one often notes that the actual measured data, although it may have the same general shape and amplitude, displays a much more complex profile shape with numerous additional inflexions. This likely reflects the fact that the actual conductor is not homogeneous but rather made-up of numerous smaller conductive lenses and stringers which, as a volume, occupy a space that can be reasonably well approximated by a single enclosing “plate”. This results is an anomaly which has a composite shape that should correspond fairly well to the plate parameters used by the modeling. It is also important to remember that the GEOTEM and

17

MEGATEM systems have a very large footprint (in the order of 400 to 500 m) and will tend to homogenize the conductive responses into a single response. This may result in depth estimates which are a bit too deep. The reporting of the depth estimates As mentioned, the fundamental model used by EMQ is the “sphere” model, although the response from a “plate” can be simulated by restricting the flow of EM currents to channel through a single plane of the sphere. However, the reader should be aware that the depth value reported by the program always refers to the top of the sphere, regardless of whether the “sphere” or “plate” model was used in the fitting. In the case of the plate model, the depth value given will reflect the top of the plate if the plate is vertical and will be close to the top of the plate for a steeply dipping plate. However, in the case of a shallow dipping or flat-lying plate, the actual depth to the plate itself will be closer to the depth value given “plus” half of the diameter of the sphere.

In the modeling results provided, if the simulated “plate” model was used in the fitting, then two depth values are given, one for the top of the “enclosing” sphere and one for the approximate depth of the plate which corresponds to the depth to the top of the sphere plus half of the diameter. The modeling approach used Like any modeling software, EMQ does not necessarily provide a unique solution. Often, several different solutions will give very comparable fits. The shape of an anomaly (comparing the differences and relative symmetries between the 2 or 3 components used, X and Z or X, Y and Z) is defined by the orientation of the body (strike, dip and offset from the flight line). Any change in these parameters will have a direct effect on the resulting shape of the anomaly such that the orientation of the body can usually be determined with very little ambiguity. The amplitude of the anomaly (and to some degree its wavelength) on the other hand, is controlled by the “conductivity-volume” and the depth to source. Here, multiple solutions can exist. A large diameter sphere of low conductivity and close to surface will give a very similar response to a much smaller diameter sphere of higher conductivity at greater depth. If one of these parameters is known, such as the diameter of the sphere or its conductivity, then the depth to source can be determined with little ambiguity. However, if all 3 parameters are unknown, then we’re back to multiple solutions.

18

The following approach to the modeling was used to reduce these ambiguities:

• Initially, 2 components (X and Z) of a given order (the 2nd order for example) were modeled in order to define the orientation of the body (strike, dip and offset from the line). On extensive axes that cross multiple survey lines, the strike was often determined directly from the map and fixed. Shorter axes or single point anomalies with less confidence on strike determined from the maps relied more on the strike determined from the modeling results.

• Then, as a second pass, having determined the orientation of the body at step 1, two or

more orders of the same component were modeled simultaneously (2nd, 3rd and 4th Moment of Z, for instance). Generally, the response from the best fitting component was used for this. The scalar differences in the amplitude of the response between the different order of moments will identify which of the alternatives is the most plausible. Since the orientation of the body cannot be determined very well from a single component, the values of dip, strike and offset obtained at step 1 were simply entered and fixed. Only the depth, diameter and the conductivity parameters were inverted.

When applicable, results from both steps are provided. *******************************************************

19

MODELING RESULTS OVER THE ADELAIDE BLOCK Conductor #: 5 Line: 40680 Anomaly: A Fiducial: 69382

Model: Plate Position: 516102 E, 5819881 N Depth to top of sphere: 125 m Diameter of the sphere: 220 m Corresponding depth to plate: 180 m Conductivity: 0.49 S/m Strike direction: 75° Dip: -30° Comments : Poor fit to the X-coil data.

-0.8

-0.0

0.8

X_02 ()

* 1.0e+000

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

1.6

3.2

Z_02 ()

* 1.0e+000

5819600 5819800 5820000 5820200Y

Cond = 0.490S/m Strike = 75.0deg Dip = -30.0deg Z = -125m Diam = 220m

-320

-240

-160

-80

Z(m)

Az = 1.2deg (Normal)

0.0

1.6

3.2

Z_02 ()

* 1.0e+000

0.0

0.8

1.6

Z_03 ()

* 1.0e+000

0.0

0.3

0.6

1.0

Z_04 ()

* 1.0e+000

5819600 5819800 5820000 5820200Y


-320

-240

-160

-80

Z(m)Az = 1.2deg (Normal)

1st pass: 2 nd Moment of X, Y, Z 2nd pass: 2nd, 3rd and 4th Moment of Z

survey data model results

20

Conductor #: 5 Line: 40690 Anomaly: A Fiducial: 68991 Model: Plate Position: 516198 E, 5819916 N Depth to top of sphere: 80 m Diameter of the sphere: 180 m Corresponding depth to plate: 90 m Conductivity: 0.72 S/m Strike direction: 75° Dip: -30° Comments :

-3.2

-1.6

-0.0

X_02 ()

* 1.0e+000

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

1.6

3.2

Z_02 ()

* 1.0e+000

5819600 5819800 5820000 5820200Y


-240

-160

-80

0

Z(m)

Az = -0.5deg (Reversed)

0.0

1.6

3.2

Z_02 ()

* 1.0e+000

0.0

0.8

1.6

Z_03 ()

* 1.0e+000

0.0

0.3

0.6

Z_04 ()

* 1.0e+000

5819600 5819800 5820000 5820200Y


-240

-160

-80

0

Z(m)




21

Conductor #: 4 Line: 40790 Anomaly: A Fiducial: 65415 Model: Plate Position: 517200 E, 5815935 N Depth to top of sphere: 55 m Diameter of the sphere: 230 m Corresponding depth to plate: 56 m Conductivity: 0.45 S/m Strike direction: 98° Dip: 96° Comments : Moderate fit for the X and Z coil data. Influence from near surface conductivity or other smaller conductive sources preventing a better fit. Similar model results obtained for adjacent line 40800.

-4.0

-2.0

0.0

2.0

X_02 ()

* 1.0e+000

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

1.6

3.2

4.8

Z_02 ()

* 1.0e+000

5815600 5815800 5816000 5816200Y

Cond = 0.450S/m Strike = 98.0deg Dip = 96.0deg Z = -55m Diam = 230m

-240

-160

-80

0

Z(m)


0.0

1.6

3.2

4.8

Z_02 ()

* 1.0e+000

0.0

0.8

1.6

Z_03 ()

* 1.0e+000

0.0

0.4

0.8

1.2

Z_04 ()

* 1.0e+000

5815600 5815800 5816000 5816200Y


-240

-160

-80

0

Z(m)




22

Conductor #: 4 Line: 40800 Anomaly: B Fiducial: 65200 Model: Plate Position: 517291 E, 5815930 N Depth to top of sphere: 65 m Diameter of the sphere: 160 m Corresponding depth to plate: 67 m Conductivity: 1.05 S/m Strike direction: 98° Dip: 103° Comments : Moderate fit for the X and Z coil data. Influence from near surface conductivity or other smaller conductive sources preventing a better fit. Similar model results obtained for adjacent line 40790.

-6.4

-3.2

-0.0

X_02 ()

* 1.0e+000

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

1.6

3.2

4.8

Z_02 ()

* 1.0e+000

5815600 5815800 5816000 5816200Y


-240

-160

-80

0

Z(m)


0.0

1.6

3.2

4.8

Z_02 ()

* 1.0e+000

0.0

0.8

1.6

Z_03 ()

* 1.0e+000

0.0

0.4

0.8

1.2

Z_04 ()

* 1.0e+000

5815600 5815800 5816000 5816200Y


-240

-160

-80

0

Z(m)




23

MODELING RESULTS OVER THE BAY BLOCK Conductor #: 1 Line: 60420 Anomaly: A Fiducial: 68480

Model: Plate Position: 547200 E, 5842711 N Depth to top of sphere: 55 m Diameter of the sphere: 460 m Corresponding depth to plate: 260 m Conductivity: 0.13 S/m Strike direction: 54° Dip: -6° Comments : Poor fit to the X-coil data. Also modeled using the sphere model (see next result).

-6.4

-3.2

-0.0

X_02 ()

* 1.0e+000

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

0.8

1.6

Z_02 ()

* 1.0e+001

5842400 5842600 5842800 5843000Y


-320

-240

-160

-80

Z(m)Az = -20.8deg (Normal)

0.0

0.8

1.6

Z_02 ()

* 1.0e+001

0.0

0.4

0.8

Z_03 ()

* 1.0e+001

0.0

2.0

4.0

6.0

Z_04 ()

* 1.0e+000

5842400 5842600 5842800 5843000Y


-320

-240

-160

-80




24

Conductor #: 1 Line: 60420 Anomaly: A Fiducial: 68480 Model: Sphere Position: 547200 E, 5842711 N Depth to top of sphere: 55 m Diameter of the sphere: 320 m Conductivity: 0.25 S/m Comments :

-6.4

-3.2

-0.0

X_02 ()

* 1.0e+000

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

0.8

1.6

Z_02 ()

* 1.0e+001

5842400 5842600 5842800 5843000Y

Cond = 0.250S/m Z = -55m Diam = 320m-240

-160

-80

0

Z(m)

Az = -20.8deg (Normal)

0.0

0.8

1.6

Z_02 ()

* 1.0e+001

0.0

0.4

0.8

Z_03 ()

* 1.0e+001

0.0

2.0

4.0

6.0

Z_04 ()

* 1.0e+000

5842400 5842600 5842800 5843000Y

Cond = 0.250S/m Z = -55m Diam = 320m-240

-160

-80

0

Z(m)




25

Conductor #: 2 Line: 60450 Anomaly: A Fiducial: 55280 Model: Plate Position: 547201 E, 5843586 N Depth to top of sphere: at surface Diameter of the sphere: 360 m Corresponding depth to plate: 120 m Conductivity: 0.22 S/m Strike direction: 58° Dip: -20° Comments : Poor fit to the X-coil data. Not able to obtain a good fit for both the X and Z coils.

-4.8

-3.2

-1.6

-0.0

1.6

X_02 ()

* 1.0e+001

-8.0

0.0

8.0

Y_02 ()

* 1.0e+001

0.0

3.2

6.4

Z_02 ()

* 1.0e+001

5843200 5843400 5843600 5843800Y

Cond = 0.220S/m Strike = 58.0deg Dip = -20.0deg Z = 0m Diam = 360m

-240

-160

-80

0

Z(m)Az = -17.4deg (Reversed)

0.0

3.2

6.4

Z_02 ()

* 1.0e+001

0.0

1.6

3.2

Z_03 ()

* 1.0e+001

0.0

0.8

1.6

2.4

Z_04 ()

* 1.0e+001

5843200 5843400 5843600 5843800Y

Cond = 0.220S/m Strike = 58.0deg Dip = -20.0deg Z = 0m Diam = 360m

-240

-160

-80

0




26

Conductor #: 1 Line: 60470 Anomaly: B Fiducial: 56932 Model: Plate Position: 547606 E, 5843052 N Depth to top of sphere: 60 m Diameter of the sphere: 444 m Corresponding depth to plate: 255 m Conductivity: 0.13 S/m Strike direction: 42° Dip: 173° Comments :

-3.2

-0.0

3.2

X_02 ()

* 1.0e+000

-8.0

0.0

8.0

Y_02 ()

* 1.0e+001

0.0

0.8

1.6

Z_02 ()

* 1.0e+001

5842500 5842750 5843000 5843250Y


-300

-200

-100

0

Z(m)


0.0

0.8

1.6

Z_02 ()

* 1.0e+001

0.0

3.2

6.4

Z_03 ()

* 1.0e+000

0.0

1.6

3.2

Z_04 ()

* 1.0e+000

5842500 5842750 5843000 5843250Y


-300

-200

-100

0

Z(m)




27

Conductor #: 8 Line: 60880 Anomaly: A Fiducial: 70225 Model: Plate Position: 551301 E, 5844913 N Depth to top of sphere: 25 m Diameter of the sphere: 360 m Corresponding depth to plate: 35 m Conductivity: 0.2 S/m Strike direction: 53° Dip: 71° Comments :

-0.8

-0.0

0.8

X_02 ()

* 1.0e+001

-16.0

-8.0

0.0

8.0

16.0

Y_02 ()

* 1.0e+000

-0.0

0.8

1.6

Z_02 ()

* 1.0e+001

5844600 5844800 5845000 5845200Y


-240

-160

-80

0

Z(m)


-0.0

0.8

1.6

Z_02 ()

* 1.0e+001

0.0

3.2

6.4

Z_03 ()

* 1.0e+000

0.0

1.6

3.2

Z_04 ()

* 1.0e+000

5844600 5844800 5845000 5845200Y


-240

-160

-80

0

Z(m)




28

Conductor #: 8 Line: 60890 Anomaly: C Fiducial: 70408 Model: Plate Position: 551386 E, 5844939 N Depth to top of sphere: 25 m Diameter of the sphere: 380 m Corresponding depth to plate: 39 m Conductivity: 0.2 S/m Strike direction: 53° Dip: -68° Comments :

-1.6

-0.8

-0.0

0.8

X_02 ()

* 1.0e+001

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

0.8

1.6

Z_02 ()

* 1.0e+001

5844500 5844750 5845000 5845250Y


-300

-200

-100

0


0.0

0.8

1.6

Z_02 ()

* 1.0e+001

0.0

3.2

6.4

Z_03 ()

* 1.0e+000

0.0

1.6

3.2

4.8

Z_04 ()

* 1.0e+000

5844500 5844750 5845000 5845250Y


-300

-200

-100

0




29


-1.6

-0.8

-0.0

0.8

X_02 ()

* 1.0e+001

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

-0.0

0.8

1.6

Z_02 ()

* 1.0e+001

5844800 5845000 5845200 5845400Y


-240

-160

-80

0

Z(m)


-0.0

0.8

1.6

Z_02 ()

* 1.0e+001

-0.0

3.2

6.4

Z_03 ()

* 1.0e+000

-0.0

1.6

3.2

Z_04 ()

* 1.0e+000

5844800 5845000 5845200 5845400Y


-240

-160

-80

0

Z(m)




30

Conductor #: 9 Line: 60960 Anomaly: C Fiducial: 65743 Model: Plate Position: 551698 E, 5846132 N Depth to top of sphere: 100 m Diameter of the sphere: 800 m Conductivity: 0.04 S/m Comments :

-1.6

-0.8

-0.0

X_02 ()

* 1.0e+001

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

3.2

6.4

Z_02 ()

* 1.0e+001

5845750 5846000 5846250 5846500Y

Cond = 0.0400S/m Z = 100m Diam = 800m-400

-300

-200

-100

0

100

Z(m)


0.0

3.2

6.4

Z_02 ()

* 1.0e+001

0.0

1.6

3.2

Z_03 ()

* 1.0e+001

0.0

0.8

1.6

Z_04 ()

* 1.0e+001

5845750 5846000 5846250 5846500Y

Cond = 0.0400S/m Z = 100m Diam = 800m-400

-300

-200

-100

0

100

Z(m)




31


-0.4

-0.0

0.4

X_02 ()

* 1.0e+001

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

3.2

6.4

Z_02 ()

* 1.0e+000

5843600 5843800 5844000 5844200Y


-240

-160

-80

0

Z(m)


0.0

3.2

6.4

Z_02 ()

* 1.0e+000

-0.0

1.6

3.2

Z_03 ()

* 1.0e+000

0.0

0.8

1.6

Z_04 ()

* 1.0e+000

5843600 5843800 5844000 5844200Y


-240

-160

-80

0

Z(m)




32


-1.6

-0.8

-0.0

0.8

X_02 ()

* 1.0e+001

-16.0

-8.0

0.0

8.0

16.0

Y_02 ()

* 1.0e+000

0.0

0.4

0.8

Z_02 ()

* 1.0e+001

5843500 5843750 5844000 5844250Y


-400

-300

-200

-100

0

100

Z(m)


0.0

0.4

0.8

Z_02 ()

* 1.0e+001

0.0

1.6

3.2

Z_03 ()

* 1.0e+000

0.0

1.6

Z_04 ()

* 1.0e+000

5843500 5843750 5844000 5844250Y


-400

-300

-200

-100

0

100

Z(m)




33

Conductor #: 11 Line: 60990 Anomaly: B Fiducial: 67511 Model: Plate Position: 552834 E, 5843895 N Depth to top of sphere: 50 m Diameter of the sphere: 385 m Corresponding depth to plate: 51 m Conductivity: 0.15 S/m Strike direction: 75° Dip: 85° Comments : Moderate fit for the X and Z coil data. Influence from near surface conductivity or other smaller conductive sources preventing a better fit.

-3.2

-0.0

3.2

X_02 ()

* 1.0e+000

-16.0

-8.0

0.0

8.0

16.0

Y_02 ()

* 1.0e+000

-0.0

1.6

3.2

Z_02 ()

* 1.0e+000

5843600 5843800 5844000 5844200Y


-400

-320

-240

-160

-80

0


-0.0

1.6

3.2

Z_02 ()

* 1.0e+000

-0.8

-0.0

0.8

1.6

Z_03 ()

* 1.0e+000

0.0

0.3

0.6

Z_04 ()

* 1.0e+000

5843600 5843800 5844000 5844200Y


-400

-320

-240

-160

-80

0

Z(m)




34

Conductor #: 10 Line: 61070 Anomaly: B Fiducial: 67483 Model: Plate Position: 553607 E, 5844112 N Depth to top of sphere: 5 m Diameter of the sphere: 176 m Corresponding depth to plate: 5 m Conductivity: 0.9 S/m Strike direction: 76° Dip: 93° Comments : Good X and Z fit. Similar results obtained for adjacent line 61080.

-3.2

-1.6

-0.0

1.6

X_02 ()

* 1.0e+001

-4.0

-2.0

0.0

2.0

Y_02 ()

* 1.0e+000

-0.0

1.6

3.2

Z_02 ()

* 1.0e+001

5843800 5844000 5844200 5844400Y


-160

-80

0

80

Z(m)


-0.0

1.6

3.2

Z_02 ()

* 1.0e+001

-0.0

0.8

1.6

Z_03 ()

* 1.0e+001

0.0

3.2

6.4

Z_04 ()

* 1.0e+000

5843800 5844000 5844200 5844400Y


-160

-80

0

80

Z(m)




35

Conductor #: 10 Line: 61080 Anomaly: C Fiducial: 68777 Model: Plate Position: 553684 E, 5844172 N Depth to top of sphere: 8 m Diameter of the sphere: 200 m Corresponding depth to plate: 8 m Conductivity: 0.66 S/m Strike direction: 76° Dip: 93° Comments : Good X and Z fit. Similar results obtained for adjacent line 61070.

-1.6

-0.0

1.6

X_02 ()

* 1.0e+001

-16.0

-8.0

0.0

8.0

16.0

Y_02 ()

* 1.0e+000

0.0

0.8

1.6

Z_02 ()

* 1.0e+001

5843800 5844000 5844200 5844400Y


-160

-80

0

80

Z(m)


0.0

0.8

1.6

Z_02 ()

* 1.0e+001

0.0

0.4

0.8

Z_03 ()

* 1.0e+001

0.0

2.0

4.0

6.0

Z_04 ()

* 1.0e+000

5843800 5844000 5844200 5844400Y


-160

-80

0

80

Z(m)




36

Conductor #: 11 Line: 61070 Anomaly: D Fiducial: 67394 Model: Plate Position: 552777 E, 5846380 N Depth to top of sphere: 20 m Diameter of the sphere: 245 m Corresponding depth to plate: 20 m Conductivity: 0.44 S/m Strike direction: 50° Dip: 93° Comments : Good X and Z fit. Similar results obtained for adjacent line 61080.

-0.8

-0.0

0.8

X_02 ()

* 1.0e+001

-16.0

-8.0

0.0

8.0

16.0

Y_02 ()

* 1.0e+000

-0.0

0.8

1.6

Z_02 ()

* 1.0e+001

5846200 5846400 5846600 5846800Y


-240

-160

-80

0


-0.0

0.8

1.6

Z_02 ()

* 1.0e+001

0.0

2.0

4.0

Z_03 ()

* 1.0e+000

0.0

1.6

3.2

Z_04 ()

* 1.0e+000

5846200 5846400 5846600 5846800Y


-240

-160

-80

0




37

Conductor #: 11 Line: 61080 Anomaly: A Fiducial: 68856 Model: Plate Position: 552842 E, 5846485 N Depth to top of sphere: 30 m Diameter of the sphere: 250 m Corresponding depth to plate: 30 m Conductivity: 0.4 S/m Strike direction: 51° Dip: 88° Comments : Good X and Z fit. Similar results obtained for adjacent line 61070.

-0.8

-0.0

0.8

X_02 ()

* 1.0e+001

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

3.2

6.4

Z_02 ()

* 1.0e+000

5846200 5846400 5846600 5846800Y


-240

-160

-80

0

Z(m)


0.0

3.2

6.4

Z_02 ()

* 1.0e+000

0.0

1.6

3.2

Z_03 ()

* 1.0e+000

0.0

0.8

1.6

Z_04 ()

* 1.0e+000

5846200 5846400 5846600 5846800Y


-240

-160

-80

0

Z(m)




38

Conductor #: 13 Line: 61320 Anomaly: E Fiducial: 73168 Model: Plate Position: 555434 E, 5846392 N Depth to top of sphere: 20 m Diameter of the sphere: 220 m Corresponding depth to plate: 62 m Conductivity: 0.55 S/m Strike direction: 40° Dip: -38° Comments : Similar results obtained with adjacent lines 61330 and 61340

-0.8

-0.0

0.8

X_02 ()

* 1.0e+001

-16.0

-8.0

0.0

8.0

16.0

Y_02 ()

* 1.0e+000

0.0

1.6

3.2

4.8

Z_02 ()

* 1.0e+001

5846200 5846400 5846600 5846800Y


-240

-160

-80

0


0.0

1.6

3.2

4.8

Z_02 ()

* 1.0e+001

0.0

1.6

Z_03 ()

* 1.0e+001

0.0

0.8

Z_04 ()

* 1.0e+001

5846200 5846400 5846600 5846800Y


-240

-160

-80

0




39

Conductor #: 13 Line: 61330 Anomaly: B Fiducial: 73371 Model: Plate Position: 555493 E, 5846521 N Depth to top of sphere: 38 m Diameter of the sphere: 310 m Corresponding depth to plate: 98 m Conductivity: 0.265 S/m Strike direction: 40° Dip: -38° Comments : Similar results obtained with adjacent lines 61320 and 61340

-6.4

-3.2

-0.0

X_02 ()

* 1.0e+000

-16.0

-8.0

0.0

8.0

16.0

Y_02 ()

* 1.0e+000

0.0

0.8

1.6

Z_02 ()

* 1.0e+001

5846200 5846400 5846600 5846800Y


-240

-160

-80

0

Z(m)


0.0

0.8

1.6

Z_02 ()

* 1.0e+001

0.0

3.2

6.4

Z_03 ()

* 1.0e+000

0.0

1.6

3.2

4.8

Z_04 ()

* 1.0e+000

5846200 5846400 5846600 5846800Y


-240

-160

-80

0

Z(m)




40

Conductor #: 13 Line: 61340 Anomaly: D Fiducial: 74544 Model: Plate Position: 555555 E, 5846633 N Depth to top of sphere: 25 m Diameter of the sphere: 285 m Corresponding depth to plate: 76 m Conductivity: 0.36 S/m Strike direction: 40° Dip: -40° Comments : Similar results obtained with adjacent lines 61320 and 61330

-0.8

-0.0

0.8

X_02 ()

* 1.0e+001

-16.0

-8.0

0.0

8.0

16.0

Y_02 ()

* 1.0e+000

0.0

1.6

3.2

4.8

Z_02 ()

* 1.0e+001

5846200 5846400 5846600 5846800Y


-240

-160

-80

0

Z(m)


0.0

1.6

3.2

4.8

Z_02 ()

* 1.0e+001

-0.0

1.6

3.2

Z_03 ()

* 1.0e+001

0.0

0.8

1.6

Z_04 ()

* 1.0e+001

5846200 5846400 5846600 5846800Y


-240

-160

-80

0

Z(m)




41


-0.0

3.2

6.4

X_02 ()

* 1.0e+000

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

0.8

1.6

Z_02 ()

* 1.0e+001

5846250 5846500 5846750 5847000Y


-300

-200

-100

0

Z(m)


0.0

0.8

1.6

Z_02 ()

* 1.0e+001

0.0

0.4

0.8

Z_03 ()

* 1.0e+001

0.0

2.0

4.0

Z_04 ()

* 1.0e+000

5846250 5846500 5846750 5847000Y


-300

-200

-100

0

Z(m)




42

Conductor #: 14 Line: 61370 Anomaly: A Fiducial: 66298 Model: Plate Position: 555908 E, 5846518 N Depth to top of sphere: 15 m Diameter of the sphere: 410 m Corresponding depth to plate: 63 m Conductivity: 0.16 S/m Strike direction: 41° Dip: -50° Comments :

-1.6

-0.8

-0.0

X_02 ()

* 1.0e+001

-8.0

0.0

8.0

Y_02 ()

* 1.0e+000

0.0

1.6

3.2

Z_02 ()

* 1.0e+001

5846250 5846500 5846750 5847000Y


-300

-200

-100

0

Z(m)


0.0

1.6

3.2

Z_02 ()

* 1.0e+001

-0.0

0.8

1.6

Z_03 ()

* 1.0e+001

0.0

3.2

6.4

Z_04 ()

* 1.0e+000

5846250 5846500 5846750 5847000Y


-300

-200

-100

0

Z(m)




43

Appendix B – EM Anomaly Listing

SYSTEM CONFIGURATION:

Pulse repetition rate....................................................90 Hz Pulse width..............................................................1931 us Offtime.....................................................................3167 us Receiver-transmitter horizontal separation.............~ -25 m Receiver-transmitter vertical separation.................~ -38 m Receiver axis orientation.....................................horizontal

MODEL USED IN FITTING: Vertical plate model Length of 600 m Depth extent of 300 m Vertical dip Strike perpendicular to flight line ANOMALY LISTING DESCRIPTION: FLT............................................................................................. ..........Flight Number LINE........................................................................................................Line Number PRT..................................................................................................Line part number AZ...................................................... ............................................Flight line heading CAT............................. ......Anomaly category N = normal, S = surficial, C = culture ID............................................................ ........................................Anomaly identifier FID................................................. ............................Fiducial value at anomaly peak CH10................................................. .........................Amplitude of channel 10 (ppm) CH12................................................ ..........................Amplitude of channel 12 (ppm) CH14.................................................. ........................Amplitude of channel 14 (ppm) CH16.................................................. ........................Amplitude of channel 16 (ppm) CH18................................................... .......................Amplitude of channel 18 (ppm) CH20.................................................... ......................Amplitude of channel 20 (ppm) NC.......................................................... .....................Number of channels deflected ALT....................................................... ............Terrain clearance of aircraft (metres) X.................................................... .......UTM X coordinate of anomaly peak (metres) Y................................................. ..........UTM Y coordinate of anomaly peak (metres)

44

Adelaide Block FLT LINE AZ CAT ID FID CH09 CH11 CH13 CH15 CH17 CH19 NC ALT X Y

533 40060 180 N A 77115.2 43 37 30 24 17 10 11 112.8 509897 5815988

533 40060 180 N B 77139.8 35 28 23 17 11 5 9 99.8 509899 5815385

533 40070 0 N A 77027.8 17 14 10 7 4 2 1 102.8 510002 5815379

533 40070 0 N B 77043.2 0 -1 -1 0 0 0 1 101.6 510004 5815779

533 40080 180 N A 76840.6 11 8 7 5 4 3 1 106.8 510088 5815382

533 40280 180 N A 73087.4 17 11 8 5 2 1 1 105.3 512096 5815935

533 40290 0 N A 72882.8 6 4 3 2 1 1 1 106.2 512197 5815932

533 40290 0 N B 72891.8 6 5 3 3 1 1 1 103.8 512199 5816187

533 40300 180 N A 72633.8 10 9 7 6 4 3 1 106.9 512295 5816307

533 40300 180 N B 72647.4 33 28 21 17 11 4 9 103.4 512294 5815984

533 40310 0 N A 72427.0 1 1 1 1 1 0 1 101.1 512389 5815982

533 40320 180 N A 72188.8 11 9 8 6 4 2 1 106.2 512497 5815991

531 40670 180 N A 74764.6 18 16 13 10 7 3 1 103.7 515999 5819945

530 40680 0 N A 69381.8 40 32 24 18 12 5 9 110.8 516102 5819874

530 40690 180 N A 68912.8 57 44 32 23 14 6 10 112.3 516198 5819872

530 40770 180 N A 66838.0 20 15 11 8 6 3 1 103.5 516993 5815889

530 40780 0 N A 66489.0 15 12 9 6 4 3 1 109.9 517104 5815890

530 40780 0 N B 66495.0 19 15 12 8 6 3 1 107.9 517099 5816075

530 40790 0 N A 65411.2 27 22 18 14 10 4 9 106.8 517200 5815824

530 40790 0 N B 65419.0 37 30 24 18 14 7 10 108.3 517201 5816068

530 40800 180 N A 65196.2 52 43 35 27 19 10 11 107.2 517291 5816031

530 40800 180 N B 65203.2 31 26 20 16 11 6 9 104.7 517291 5815836

530 40810 0 N A 64612.2 19 15 11 7 4 1 1 104.8 517401 5815815

530 40810 0 N B 64619.4 28 21 16 12 8 3 3 106.3 517402 5816037

530 40820 180 N A 64392.2 11 9 6 5 3 2 1 114.7 517501 5816114

530 40820 180 N B 64405.0 20 15 10 6 3 1 1 105.8 517497 5815756

529 40830 180 N A 58313.8 15 11 8 5 4 2 1 111.5 517602 5816096

529 40830 180 N B 58324.0 29 20 13 9 5 2 1 108.4 517606 5815810

529 40840 0 N A 57740.4 23 15 9 6 3 1 1 115.6 517695 5815848

529 40840 0 N B 57748.6 5 3 1 0 0 0 1 116.3 517698 5816104

529 40850 180 N A 57522.0 11 7 5 3 1 0 1 113.2 517802 5816069

529 40850 180 N B 57531.4 27 18 12 6 3 0 1 106.9 517804 5815813

529 40860 0 N A 56944.8 9 7 4 3 2 0 1 109.1 517904 5815750

529 40860 0 N B 56954.4 11 7 4 3 1 1 1 107.5 517904 5816041

534 49080 270 N A 59323.2 47 40 32 25 19 9 10 103.6 517286 5816005

534 49080 270 N B 59488.6 15 13 11 8 6 2 1 107.7 512356 5816002

534 49080 270 N C 59571.8 25 21 18 15 11 6 1 113.4 509905 5816000

45

Bay Block FLT LINE AZ CAT ID FID CH09 CH11 13 CH15 CH17 CH19 NC ALT X Y 44 60370 160 N A 64136.0 23 17 11 7 3 1 1 103 546946 5841930 44 60400 340 N A 66953.4 28 24 18 15 11 5 9 112 547008 5842633 44 60410 160 N A 67180.0 68 58 46 37 26 12 11 109 547129 5842610 44 60420 340 N A 68479.6 203 171 140 112 81 44 12 102.9 547208 5842693 44 60430 160 N A 68693.0 403 354 303 252 192 105 12 105.1 547322 5842662 44 60440 340 N A 69969.2 173 153 130 109 84 46 12 104.4 547401 5842746 44 60440 340 N B 69999.4 74 66 54 47 37 23 2 105.2 547095 5843597 45 60450 160 N A 55280.6 509 445 382 318 248 153 12 99.8 547203 5843580 45 60450 160 N B 55301.8 117 100 84 69 52 29 12 100 547431 5842959 45 60460 340 N A 56709.6 198 167 136 107 75 35 12 110.8 547519 5843019 45 60460 340 N B 56736.2 379 335 291 250 202 131 12 111.8 547275 5843671 45 60470 160 N A 56910.0 43 37 32 27 22 13 12 107.8 547377 5843673 45 60470 160 N B 56932.6 196 167 137 109 76 34 12 110.3 547609 5843041 45 60480 340 N A 58326.2 101 87 75 62 47 25 12 109.9 547696 5843095 45 60490 160 N A 58542.2 22 19 16 14 11 8 1 109.2 547785 5843161 45 60520 340 N A 61576.2 23 19 14 10 7 4 1 106.8 547908 5843694 46 60530 160 N A 65098.4 11 8 5 4 2 1 1 107.3 548014 5843658 46 60540 340 N A 66500.2 12 8 4 2 0 0 1 102.6 548124 5843697 46 60550 160 N A 66688.0 28 20 13 8 4 1 1 107.6 548198 5843760 46 60560 340 N A 68067.0 27 19 11 6 3 0 1 106 548297 5843790 46 60570 160 N A 68255.4 23 17 11 7 3 1 1 102 548391 5843822 46 60580 340 N A 69622.4 6 3 0 -1 -1 -2 1 107.8 548468 5843929 47 60640 340 N A 58143.6 13 12 8 7 4 2 1 108.3 548767 5844829 47 60650 160 N A 58278.0 15 12 8 8 5 2 1 108.5 548867 5844865 47 60660 340 N A 59766.4 19 17 12 10 7 3 1 105.5 548951 5844933 47 60670 160 N A 59898.6 24 20 14 12 8 3 1 107.2 549025 5845007 47 60680 340 N A 61372.6 14 13 10 8 5 2 1 105 549088 5845140 48 60690 160 N A 64850.0 16 13 10 8 5 3 1 109.8 549157 5845221 48 60700 340 N A 66253.0 24 20 16 14 10 5 1 102 550115 5842888 48 60710 160 N A 66548.4 27 23 18 15 11 4 9 107.1 550200 5842951 48 60710 160 N B 66553.4 56 46 35 28 17 6 10 106 550250 5842806 48 60720 340 N A 67854.6 26 21 16 13 8 2 1 99.5 550350 5842829 48 60720 340 N B 67859.6 37 30 23 18 11 4 9 97.2 550301 5842957 49 60780 340 N A 58800.6 15 11 7 5 3 1 1 102 550492 5844200 49 60790 160 N A 59012.6 48 34 22 14 6 0 8 107.6 550582 5844211 49 60800 340 N A 60383.8 34 22 12 6 2 0 3 102.1 550698 5844218 80 60810 340 N A 75585.4 5 3 1 1 0 -1 1 111.6 550773 5844324 49 60840 340 N A 63554.8 71 58 45 35 26 13 11 103.1 550806 5845075 50 60850 160 N A 67182.6 61 47 35 25 16 7 10 108.6 550897 5845144 50 60850 160 N B 67189.8 25 21 15 12 7 3 1 110.1 550982 5844924 50 60860 340 N A 68607.2 31 26 20 16 11 6 9 108 551073 5844951 50 60860 340 N B 68620.6 74 54 38 26 15 6 10 110.2 550955 5845275 50 60870 160 N A 68781.0 142 98 64 40 21 8 10 104.1 551061 5845276

46

FLT LINE AZ CAT ID FID CH09 CH11 13 CH15 CH17 CH19 NC ALT X Y 50 60870 160 N B 68791.8 77 65 55 45 34 19 12 107.4 551182 5844947 50 60880 340 N A 70221.6 33 29 24 22 16 10 5 107.4 551332 5844814 50 60880 340 N B 70231.0 123 105 88 73 56 32 12 107.6 551258 5845038 50 60880 340 N C 70246.2 80 58 39 28 17 7 10 103.6 551126 5845398 50 60890 160 N A 70385.8 63 50 37 29 20 10 11 111 551143 5845617 50 60890 160 N B 70404.6 156 132 107 88 65 37 12 103.1 551349 5845055 50 60890 160 N C 70412.6 43 37 30 25 19 10 11 108.4 551429 5844809 50 60900 340 N A 71807.8 56 48 40 34 25 15 12 110.8 551495 5844941 50 60900 340 N B 71817.6 135 111 89 71 50 24 12 108.3 551411 5845176 50 60900 340 N C 71829.4 83 66 52 40 27 12 11 108.8 551303 5845461 50 60900 340 N D 71843.2 126 104 83 66 48 24 12 103.5 551185 5845812 50 60910 160 N A 71958.0 200 168 139 112 82 42 12 109 551278 5845811 50 60910 160 N B 71979.0 157 130 104 82 59 29 12 108 551521 5845168 50 60910 160 N C 71985.6 54 46 37 31 23 12 11 106.7 551596 5844964 50 60920 340 N A 73366.6 55 46 38 31 22 11 11 111.4 551668 5845075 50 60920 340 N B 73374.6 113 92 72 56 39 18 12 104.9 551595 5845277 50 60920 340 N C 73401.4 373 313 257 206 151 78 12 98.8 551346 5845937 51 60930 160 N A 62642.6 745 622 510 406 294 148 12 100 551462 5845918 51 60930 160 N B 62665.4 53 38 28 22 15 8 10 105.4 551686 5845298 51 60930 160 N C 62673.0 34 30 25 20 15 7 10 106 551762 5845096 51 60940 340 N A 64031.4 32 23 14 9 4 1 3 103.2 552380 5843682 51 60940 340 N B 64037.8 16 10 6 4 1 1 1 101.6 552312 5843862 51 60940 340 N C 64095.4 32 23 16 13 9 4 3 110.4 551740 5845434 51 60940 340 N D 64116.2 762 641 524 417 301 149 12 104.4 551539 5846001 51 60950 160 N A 64260.0 831 702 579 463 335 166 12 105.7 551642 5846013 51 60950 160 N B 64339.4 39 27 18 12 6 2 8 101.2 552420 5843864 51 60950 160 N C 64346.6 74 52 35 23 13 4 9 104 552491 5843673 51 60960 340 N A 65649.0 92 71 53 38 24 11 11 108.7 552569 5843754 51 60960 340 N B 65657.2 42 33 24 18 11 5 9 107 552484 5843985 51 60960 340 N C 65734.4 742 629 519 416 301 146 12 108 551698 5846132 51 60970 160 N A 65858.2 409 341 277 219 156 74 12 108.8 551801 5846154 51 60970 160 N B 65941.4 70 56 41 31 20 9 10 106.1 552602 5843946 51 60970 160 N C 65949.2 119 94 71 53 34 14 11 104 552674 5843740 51 60980 340 N A 67218.8 152 119 88 64 40 17 12 99.8 552746 5843838 51 60980 340 N B 67225.4 90 69 51 36 22 8 10 101.4 552682 5844021 51 60980 340 N C 67307.4 227 188 152 121 88 46 12 104.5 551861 5846293 51 60990 160 N A 67415.6 155 129 104 82 58 29 12 110.3 551886 5846515 51 60990 160 N B 67507.2 61 47 35 25 14 5 9 107.3 552788 5844012 51 60990 160 N C 67514.8 81 62 45 32 18 5 10 107.9 552868 5843809 51 61000 340 N A 68785.2 59 45 32 22 12 5 10 101.7 552941 5843882 51 61000 340 N B 68793.8 31 23 15 11 6 2 3 102.1 552859 5844117 51 61000 340 N C 68886.2 144 119 95 74 51 25 12 107 551950 5846623 63 61010 160 N A 66990.8 140 112 86 65 44 20 12 106.1 552066 5846618 63 61010 160 N B 67078.0 43 35 28 23 16 8 10 107.8 552997 5844050 63 61010 160 N C 67085.0 62 50 39 30 21 9 10 108.5 553065 5843837 63 61020 340 N A 68364.4 124 102 79 62 42 17 12 106.4 553126 5843947 63 61020 340 N B 68370.8 76 64 51 41 28 11 11 107.2 553065 5844123 63 61020 340 N C 68472.4 121 93 68 49 30 10 11 106.6 552072 5846859

47

FLT LINE AZ CAT ID FID CH09 CH11 13 CH15 CH17 CH19 NC ALT X Y 63 61030 160 N A 68563.4 130 97 68 47 27 9 10 106.1 552202 5846841 63 61030 160 N B 68658.0 105 89 74 60 43 19 12 109.3 553183 5844079 63 61030 160 N C 68664.6 98 83 69 56 39 17 12 110.1 553255 5843884 63 61040 340 N A 69960.6 187 160 133 108 80 42 12 108.5 553322 5843983 63 61040 340 N B 69967.0 156 134 111 90 68 32 12 107.8 553260 5844152 63 61040 340 N C 70070.0 119 87 61 41 25 8 10 105.4 552237 5846957 63 61050 160 N A 70164.0 48 37 25 18 10 3 9 105.3 552414 5846837 63 61050 160 N B 70178.8 29 26 21 17 12 7 9 105.7 552555 5846425 63 61050 160 N C 70261.0 194 168 141 117 87 46 12 110.7 553389 5844121 63 61050 160 N D 70266.4 207 179 149 123 92 46 12 111.5 553448 5843961 63 61060 340 N A 71559.6 279 243 208 173 133 75 12 104.2 553514 5844046 63 61060 340 N B 71565.2 250 218 186 155 119 66 12 105.9 553462 5844187 63 61060 340 N C 71649.6 33 29 24 20 15 8 2 105.3 552715 5846282 63 61060 340 N D 71657.2 89 76 63 51 38 19 12 105.6 552641 5846476 63 61060 340 N E 71674.2 39 29 21 15 9 4 8 112.8 552485 5846901 65 61070 160 N A 67389.2 101 86 72 59 43 24 12 111.4 552738 5846489 65 61070 160 N B 67397.2 59 52 46 39 30 17 12 108.5 552809 5846293 65 61070 160 N C 67480.8 215 190 164 141 113 69 12 106.1 553586 5844168 65 61070 160 N D 67485.4 169 149 128 109 86 51 12 107.1 553631 5844050 65 61080 340 N A 68775.2 137 117 98 81 62 33 12 104.8 553710 5844101 65 61080 340 N B 68780.0 214 182 152 124 91 48 12 105.4 553659 5844244 65 61080 340 N C 68854.0 81 69 57 47 35 18 12 105.6 552872 5846408 65 61080 340 N D 68860.6 102 83 66 50 33 14 11 107.6 552798 5846605 53 61090 160 N A 71622.6 101 81 61 46 28 10 10 106.6 552903 5846616 53 61090 160 N B 71630.8 50 40 32 25 16 6 10 108.8 552989 5846394 53 61090 160 N C 71709.4 75 64 54 45 33 18 12 106.3 553777 5844235 53 61090 160 N D 71715.4 43 36 29 24 19 11 11 107 553836 5844073 53 61100 340 N A 72967.0 71 62 52 45 36 23 12 103.8 553912 5844151 53 61100 340 N B 72971.8 149 130 111 94 75 47 12 103 553862 5844285 53 61100 340 N C 72978.8 60 51 42 35 28 17 5 100 553791 5844481 53 61100 340 N D 73052.2 51 41 31 23 15 5 10 111.2 553045 5846537 53 61100 340 N E 73059.4 93 75 57 42 25 9 10 109.8 552973 5846740 53 61110 160 N A 73157.4 24 18 12 9 7 2 1 107.3 553086 5846728 53 61110 160 N B 73164.2 31 25 18 14 10 4 9 111.5 553152 5846544 53 61110 160 N C 73238.8 136 115 95 77 58 32 12 108.9 553904 5844472 53 61110 160 N D 73245.6 102 87 72 60 46 28 12 107.3 553969 5844283 53 61110 160 N E 73251.2 59 49 41 34 26 16 12 104.9 554024 5844123 53 61120 340 N A 74473.8 29 25 19 16 11 7 9 101.2 554100 5844201 53 61120 340 N B 74480.2 51 42 34 27 20 10 11 104.6 554035 5844381 53 61120 340 N C 74485.6 71 60 49 40 30 16 12 104.2 553978 5844532 65 61130 160 N A 69098.0 21 18 14 13 8 5 1 108.1 554096 5844529 65 61170 160 N A 72532.6 27 21 16 12 8 5 1 111 554454 5844694 65 61180 340 N A 73786.0 38 30 22 16 10 6 9 110.4 554507 5844828 66 61190 160 N A 59334.2 71 61 49 40 28 12 11 107 554603 5844859 66 61200 340 N A 60523.6 31 25 19 16 11 5 9 107.8 554768 5844725 66 61200 340 N B 60533.4 72 62 51 41 29 14 12 106.5 554674 5844992 66 61210 160 N A 60805.6 60 50 41 34 26 12 11 108.3 554770 5845017 66 61210 160 N B 60815.4 21 17 14 12 8 5 1 107.7 554878 5844724

48

FLT LINE AZ CAT ID FID CH09 CH11 13 CH15 CH17 CH19 NC ALT X Y 66 61220 340 N A 61982.2 30 25 20 16 12 6 9 104 554923 5844859 66 61220 340 N B 61996.4 43 37 32 26 19 9 10 104.3 554806 5845232 66 61230 160 N A 62248.2 48 42 35 30 22 11 11 112.7 554892 5845281 66 61230 160 N B 62263.2 23 19 15 12 9 4 1 110.8 555041 5844833 66 61240 340 N A 63457.0 44 40 34 29 21 12 2 110.2 554955 5845413 66 61250 160 N A 63721.0 60 53 46 38 29 17 12 108.7 555040 5845424 66 61250 160 N B 63733.4 21 18 13 10 7 4 1 109.6 555170 5845064 80 61260 160 N A 74043.4 64 55 47 40 31 17 12 111.1 555123 5845508 80 61260 160 N B 74052.2 12 10 9 7 5 3 1 112.4 555211 5845255 80 61260 160 N C 74082.6 21 15 11 9 6 1 1 111.9 555531 5844386 80 61260 160 N D 74097.6 9 2 1 1 0 0 1 116.1 555687 5843946 67 61270 160 N A 69156.6 61 50 42 34 25 13 11 102.7 555172 5845669 67 61270 160 N B 69172.0 22 18 14 12 9 5 1 106.7 555341 5845206 67 61270 160 N C 69199.0 45 36 28 23 16 7 10 103.2 555648 5844389 67 61270 160 N D 69209.6 21 12 8 7 5 3 1 107.4 555764 5844060 67 61280 340 N A 70251.2 58 41 29 23 15 6 10 105.4 555796 5844251 67 61280 340 N B 70261.2 66 52 40 31 21 9 10 110.8 555711 5844509 67 61280 340 N C 70299.0 25 20 17 14 11 5 1 108.2 555347 5845458 67 61280 340 N D 70313.6 60 46 36 27 18 9 10 105.9 555229 5845824 67 61290 160 N A 70556.0 99 75 55 39 23 9 10 106.3 555324 5845843 67 61290 160 N B 70566.8 19 15 11 9 6 3 1 108.9 555445 5845512 67 61290 160 N C 70600.8 78 60 44 32 21 8 10 109.3 555811 5844461 67 61290 160 N D 70608.0 69 49 36 28 18 7 10 110.6 555893 5844243 67 61300 340 N A 71655.2 72 49 35 27 17 7 10 111.7 555982 5844317 67 61300 340 N B 71665.4 71 56 44 34 23 10 11 109.7 555880 5844570 67 61300 340 N C 71707.4 31 24 18 15 9 4 8 109.5 555493 5845643 67 61300 340 N D 71719.4 101 71 48 32 17 6 10 107.5 555396 5845940 67 61310 160 N A 71959.0 51 33 20 13 5 -2 7 107.2 555498 5845980 67 61310 160 N B 71967.2 18 12 9 7 3 1 1 111.3 555585 5845733 67 61310 160 N C 72006.0 70 53 42 33 22 9 11 108.6 555993 5844570 67 61310 160 N D 72016.2 55 34 23 18 11 4 9 110.1 556103 5844265 67 61320 340 N A 73086.2 41 21 12 7 4 2 3 108.9 556187 5844311 67 61320 340 N B 73098.0 46 33 23 17 11 4 9 110.4 556079 5844602 67 61320 340 N C 73147.8 23 17 12 9 5 2 1 111.5 555628 5845858 67 61320 340 N D 73160.0 24 16 10 7 4 1 1 111.3 555514 5846170 67 61320 340 N E 73171.0 184 153 126 104 79 45 12 105.3 555412 5846455 67 61320 340 N F 73189.0 23 19 15 12 7 3 1 109.4 555253 5846910 67 61330 160 N A 73356.0 33 25 19 14 8 2 8 110.2 555333 5846969 67 61330 160 N B 73372.0 138 118 100 83 63 34 12 109.3 555499 5846504 67 61330 160 N C 73378.8 29 20 14 11 7 3 1 110.6 555571 5846306 67 61330 160 N D 73434.4 30 20 13 10 6 2 1 114.2 556176 5844693 67 61330 160 N E 73447.4 22 7 1 0 0 1 1 107.5 556308 5844308 67 61340 340 N A 74458.2 20 10 6 4 2 0 1 113.3 556362 5844444 67 61340 340 N B 74468.8 29 19 12 9 5 3 1 108.6 556253 5844712 67 61340 340 N C 74534.8 33 24 17 13 8 3 5 113.8 555641 5846372 67 61340 340 N D 74544.2 386 335 286 239 185 103 12 111 555560 5846617 67 61340 340 N E 74562.8 62 47 35 25 15 4 9 112.4 555398 5847100 67 61350 160 N A 74735.2 156 119 87 60 34 8 10 109 555517 5847037

49

FLT LINE AZ CAT ID FID CH09 CH11 13 CH15 CH17 CH19 NC ALT X Y 67 61350 160 N B 74750.0 124 107 89 75 56 29 12 109.6 555666 5846609 67 61350 160 N C 74754.0 171 141 115 91 65 30 12 109.1 555707 5846493 67 61350 160 N D 74815.0 22 13 8 6 3 0 1 108.9 556357 5844716 67 61350 160 N E 74822.2 15 7 4 4 3 3 1 107.9 556432 5844503 67 61360 340 N A 75824.0 11 5 3 2 1 -1 1 107.7 556533 5844522 67 61360 340 N B 75837.4 9 5 4 4 2 0 1 103.6 556409 5844859 67 61360 340 N C 75905.8 285 227 176 132 88 36 12 111.4 555790 5846560 67 61360 340 N D 75928.6 35 28 21 17 11 3 9 108 555573 5847157 69 61370 160 N A 66295.4 345 280 223 172 118 53 12 107.5 555886 5846583 69 61380 340 N A 67422.0 40 34 27 24 16 8 5 109.4 556021 5846519 69 61390 160 N A 67516.4 25 21 17 14 10 4 1 106.1 556130 5846552 71 61550 160 N A 74093.2 19 14 10 7 2 1 1 112.8 560665 5838711 80 69011 70 N A 73539.6 171 141 114 90 64 28 12 114.5 551722 5846414 80 69011 70 N B 73585.0 37 28 21 15 9 3 8 112 552884 5846832 80 69020 250 N A 72680.2 66 56 46 38 27 13 11 118.5 555730 5846799 80 69020 250 N B 72688.4 69 63 56 49 39 21 2 111.3 555516 5846718 80 69020 250 N C 72844.2 123 98 78 62 44 21 12 108.3 551461 5845255 80 69020 250 N D 72850.6 116 91 70 54 37 17 12 107.2 551283 5845191 80 69020 250 N E 72860.2 61 47 35 26 17 8 10 107.7 551015 5845089 80 69020 250 N F 72867.6 40 30 22 16 10 3 9 106.9 550809 5845014 80 69020 250 N G 73003.2 138 124 109 95 77 48 12 111.5 547193 5843708 80 69030 70 N A 71592.2 474 414 354 295 225 117 12 111.9 547343 5842699 80 69030 70 N B 71604.4 49 37 28 20 11 5 9 108.9 547657 5842808 80 69030 70 N C 71893.8 69 59 50 41 31 16 12 113.4 555111 5845509 80 69030 70 N D 71910.6 22 16 10 7 3 2 1 113.3 555587 5845684

50

King Block FLT LINE AZ CAT ID FID CH09 CH11 CH13 CH15 CH17 CH19 NC ALT X Y

526 51110 210 N A 54518.8 3 1 0 0 0 0 1 98.2 560116 5863593

526 51110 210 N B 54538.2 4 2 1 1 0 0 1 100.5 559897 5863202

526 51120 30 N A 54820.4 4 2 1 0 0 0 1 107.4 559948 5863080

526 51120 30 N B 54837.8 5 3 2 1 0 1 1 108.5 560239 5863607

526 51130 210 N A 55281.6 3 1 0 0 0 0 1 101.8 560279 5863468

526 51130 210 N B 55307.4 3 1 0 0 0 0 1 109.2 559982 5862949

526 51140 30 N A 55578.2 6 3 2 1 0 0 1 103.2 560050 5862858

526 51140 30 N B 55595.0 4 2 1 1 0 0 1 104.6 560327 5863359

526 51150 210 N A 56037.0 2 0 0 -1 -1 0 1 101.7 560402 5863274

526 51150 210 N B 56059.2 5 2 1 1 1 0 1 107.7 560133 5862817

526 51160 30 N A 56322.4 4 2 0 0 0 0 1 107.4 560245 5862803

526 51160 30 N B 56335.6 5 2 1 1 1 0 1 109.2 560463 5863198

526 51170 210 N A 56781.2 3 1 1 0 0 0 1 103 560575 5863159

526 51170 210 N B 56800.2 5 2 1 0 0 1 1 103.9 560343 5862759

526 51180 30 N A 57058.8 5 3 1 1 0 0 1 103.6 560439 5862753

526 51180 30 N B 57072.4 6 3 1 0 0 0 1 106.8 560680 5863163

526 51190 210 N A 57508.0 7 3 1 0 0 0 1 101.2 560763 5863122

526 51190 210 N B 57528.2 7 3 1 1 0 0 1 101.7 560526 5862693

526 51200 30 N A 57801.0 11 6 3 2 2 1 1 109.4 560620 5862648

526 51200 30 N B 57815.6 9 5 3 2 1 2 1 120.3 560861 5863077

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