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P-06-81
Forsmark site investigation
Comparative geological logging with the Boremap system: 176.5–360.9 m of borehole KFM06C
Jesper Petersson, Göran Skogsmo, Johan Berglund
SwedPower AB
Allan Stråhle, Geosigma AB
May 2006
Svensk Kärnbränslehantering ABSwedish Nuclear Fueland Waste Management CoBox 5864SE-102 40 Stockholm Sweden Tel 08-459 84 00 +46 8 459 84 00Fax 08-661 57 19 +46 8 661 57 19
CM
Gru
ppen
AB
, Bro
mm
a, 2
006
ISSN 1651-4416
SKB P-06-81
Forsmark site investigation
Comparative geological logging with the Boremap system: 176.5–360.9 m of borehole KFM06C
Jesper Petersson, Göran Skogsmo, Johan Berglund
SwedPower AB
Allan Stråhle, Geosigma AB
May 2006
Keywords: KFM06C, Geology, Drill core, Comparative mapping, BIPS, Boremap, Fractures, Forsmark, AP PF 400-05-086.
This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the authors and do not necessarily coincide with those of the client.
A pdf version of this document can be downloaded from www.skb.se
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Abstract
This report presents the results from four days of geological mapping of KFM06C, a 1 km long telescopic borehole in the Forsmark area, by using the Boremap system. The mapping is part of a project initiated to evaluate possible differences in the geological judgement and the methodology used for the drill core logging at Forsmark and subarea Laxemar site investigation areas. During the four days period, an interval from 176.5 to 360.9 metres of KFM06C was mapped. All lithological features that occur within this interval have been registered and documented with the same criteria used by the SwedPower team during the regular geological logging of boreholes in the Forsmark area.
The 184.4 metres long interval of KFM06C is dominated by a medium-grained metagranite. Other frequent rock types in the interval include pegmatitic granite, amphibolite, aplitic metagranite and fine- to finely medium-grained granite. None of these occurrences exceed a few metres in length along the borehole. Virtually all rocks have experienced Svecofennian metamorphism under amphibolite facies conditions. Structurally, the rocks are characterised by composite L-S fabrics, with a slight predominance of linear mineral fabrics. Seven minor zones of more intense ductile deformation have been registered in the mapped interval of KFM06C. A faint to weak oxidation of feldspars is generally associated with more intensely fractured intervals.
The total number of fractures registered in the 184.4 metres long interval of KFM06C amounts to 646. Of these are 219 open, 14 partly open and 413 sealed. Two rather narrow crush zones occur in the mapped interval. Three fracture sets may be distinguished. (1) Horizontal to sub-horizontal fractures that are mostly open. The maximum aperture of these fractures is 4 millimetres. The most frequent infilling minerals are calcite, chlorite and clay minerals. (2) Steeply dipping fractures, striking roughly N–S. Most of these fractures are inferred to be sealed. Typical infilling minerals are calcite, chlorite, hematite, adularia, laumontite, quartz and pyrite. (3) Sealed, vertical to sub-vertical fractures with ENE–WSW strike. They are mainly restricted to the length interval below ca 280 metres. The majority is sealed by adularia, calcite and chlorite.
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Sammanfattning
Föreliggande rapport redovisar resultaten från fyra dagars Boremapkartering av KFM06C, ett 1 km djupt teleskopborrhål i Forsmarksområdet. Karteringen ingår i ett projekt för att utvärdera eventuella skillnader i geologiska bedömningar och metodiken som används vid borrkärnekartering i undersökningsområde Forsmark respektive delområde Laxemar. Under fyradagarsperioden karterades ett längdintervall från 176,5 till 360,9 meter av KFM06C. Alla strukturer och litologiska enheter som förekommer i intervallet registrerades och dokumenterades med samma kriterier som används av SwedPowers geologer vid den reguljära borrhålskarteringen i Forsmark.
Det 184,4 meter långa intervallet i KFM06C domineras av en medelkornig metagranit. Andra vanligt förekommande bergarter i intervallet är pegmatitisk granit, amfibolit, aplitisk metagranit och fin- till fint medelkornig granit. Enskilda förekomster uppgår aldrig till mer än några meters borrhålslängd. I det närmaste alla bergarter har genomgått Svekofennisk amfibolitfacies-metamorfos. Bergarterna karaktäriseras av en sammansatt L-S-struktur, med en något tydligare mineralstänglighet. Sju mindre zoner med mer kraftig duktil deformation har registrerats i det karterade intervallet av KFM06C. En svag till mycket svag oxidation av fältspater uppträder normalt i längdintervall som är mer kraftigt uppspruckna.
Det totala antalet sprickor som registrerats i det 184,4 meter långa intervallet av KFM06C uppgår till 646. Av dessa är 219 öppna, 14 partiellt öppna och 413 läkta. Två mindre krosszoner förekommer i det karterade intervallet. Tre sprickgrupper kan urskiljas. (1) Horisontella till subhorisontella sprickor som till största delen är öppna. Den maximala aperturen hos dessa uppgår till 4 millimeter. De vanligast förekommande sprickfyllnads-mineralen är kalcit, klorit och lermineral. (2) Brant stupande sprickor som stryker ungefär N–S. De flesta av dessa sprickor bedöms vara läkta. Typiska sprickmineral inkluderar kalcit, klorit, hematit, adularia, laumontit, kvarts och pyrit. (3) Läkta, vertikala till sub-vertikala sprickor som stryker ENE–VSV. De är huvudsakligen begränsade till ett längd-intervall under ca 280 meter. Majoriteten av dem är läkta med adularia, kalcit och klorit.
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Contents
1 Introduction 7
2 Objectiveandscope 9
3 Equipment 113.1 Description of equipment/interpretation tools 11
4 Execution 134.1 General 134.2 Preparations 134.3 Data handling 134.4 Analyses and interpretations 144.5 Nonconformities 14
5 Results 175.1 Core lithology 175.2 Ductile structures 175.3 Alteration 185.4 Fractures 18
5.4.1 Fracture frequencies and orientations 185.4.2 Fracture mineralogy 19
Appendix1 WellCAD image 21Appendix2 Borehole diameters 25Appendix3 Downhole deviation measurements 27Appendix4 Length reference marks 39
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1 Introduction
Since 2002, SKB investigates two potential sites at Forsmark and Oskarshamn, for a deep repository in the Swedish Precambrian basement. In order to characterise the bedrock down to a depth of about 1 km at the two site investigation areas, SKB launched several extensive drilling programmes. A detailed geological logging of the drill cores obtained through the drilling programs is essential for subsequent sampling and borehole investigations, and consequently, for the three-dimensional modelling of the two sites. For this purpose, the so-called Boremap system has been developed. The system integrates results from geologi-cal drill core logging, or alternatively, the drill cuttings when a core is not available, with information from BIPS-logging (Borehole Image Processing System) and calculates the absolute position and orientation of fractures and various planar lithological features (SKB MD 143.006 and 146.005).
To assure the comparability between the two site investigation areas, it is essential that there is a general consensus in the geological judgements and the methodology used for the drill core logging. The subject has arisen as the geologists involved in the logging have been strictly tied to one of the site investigation areas, and the exchange of experiences is rather limited. In order to evaluate possible differences in the mapping, SKB initiated a project where the core logging teams at the two sites were switching locality to work with a drill core from the other site investigation area. The two boreholes chosen for the mapping were telescopic drilled borehole KFM06C from the Forsmark site investigation area and core drilled borehole KLX07B from the subarea Laxemar, which is part of the Simpevarp site investigation area at Oskarshamn.
This document reports the results from the comparative geological logging of borehole KFM06C performed by geologists from SwedPower AB. The activity is part of the site investigation at Forsmark. The work was carried out in accordance with activity plan AP PF 400-05-086. In Table 1-1 controlling documents for performing this activity are listed. Both activity plan and method descriptions are SKB’s internal controlling documents.
Table1‑1. Controllingdocumentsfortheperformanceoftheactivity.
Activityplan Number Version
Jämförande Boremapkartering på del av teleskopborrhål KFM06C och KLX07B
AP PF 400-05-086 1.0
Methoddocuments Number VersionMetodbeskrivning för Boremap-kartering SKB MD 143.006 2.0Nomenklatur vid Boremap-kartering SKB MD 143.008 1.0Mätsystembeskrivning för Boremapkartering, Boremap v 3.0 SKB MD 146.005 1.0
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2 Objectiveandscope
Borehole KFM06C is a ca 1 km long, telescopic borehole drilled in the northern part of the Forsmark site investigation area with 60° inclination towards NNE (026°). It starts with percussion drilling (Ø = 251 mm) to a length of 100.40 metres, followed by core drilling at Ø = 86 millimetres to a length of 102.08 metres, and at Ø = 77 millimetres down to full borehole length at 1,000.43 metres. The diameters of the two drill cores are 70 and 51 millimetres, respectively, under ideal conditions. The available BIPS-image of KFM06C covers the core drilled length interval at Ø = 77 millimetres.
The comparative geological logging of KFM06C starts at 176.5 metres adjusted length, and should proceed for 4×8 hours. This includes 15–20 minutes of daily mapping controls by examination of Boremap generated variable/summary reports and a WellCad log to match. The length of the interval, which was mapped during the four days, amounts to 184.4 metres (176.5–360.9 meters). All structures and lithologies that occur within this interval have been registered and documented with the same criteria used by the SwedPower team during the regular geological logging of the boreholes in the Forsmark area.
11
3 Equipment
3.1 Descriptionofequipment/interpretationtoolsAll BIPS-based mapping was performed in Boremap v 3.6. This software contains the bedrock and mineral standard used by the Geological Survey of Sweden (SGU) for geologi-cal mapping of the surface at the Forsmark site investigation area, to enable correlation with the surface geology. Additional software used during the course of the geological logging was BIPS Viewer v 1.10 and Microsoft Access. The final data presentation was made by Geoplot and WellCAD v 3.2.
The following equipment was used to facilitate the core logging: folding rule, concentrated hydrochloric acid diluted with three parts of water, unglazed porcelain plate, knife, hand lens, paintbrush and tap water.
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4 Execution
4.1 GeneralDuring the core logging, the ca 900 metres drill core obtained from the interval 102.08–1,000.43 metres of KFM06C was available in its full length on roller tables in the core-mapping accommodation at Forsmark (the Llentab hall, near the SKB/SFR-office). No thin-sections were available from the drill cores, and all lithological descriptions are based on ocular inspection. The mapping was done by two geologists; one did the core logging while the other registered the information in Boremap.
The core logging of KFM06C was performed in Boremap v 3.6 according to activity plan AP PF 400-05-086 (SKB internal document) following the SKB method description/instruc-tion for Boremap mapping, SKB MD 143.006 (v 2.0) and 143.008 (v 1.0). A WellCAD summary of the mapping is presented in Appendix 1.
4.2 PreparationsThe length registered in the BIPS-image deviates from the true borehole length with increasing depth, and the difference at the bottom of KFM06C is about 5 metres. It was, therefore, necessary to adjust the length in KFM06C with reference to groove millings cut into the borehole wall at every 50 metres. The precise level of each reference mark can be found in SKB’s database SICADA (Appendix 4). This adjustment was done already during the start of the regular mapping of KFM06C. Consequently, it was copied directly into the database used for the comparative mapping.
Data necessary for calculations of absolute orientation of structures in the borehole includes borehole diameter, azimuth and inclination, and these data were imported directly from SKB’s database SICADA (Appendices 2 and 3).
4.3 DatahandlingTo obtain the best possible data security, the mapping was performed on the SKB intranet, with regular back-ups on the local drives.
To avoid that any broken fractures become unregistered, the number of broken fractures in the drill core was regularly checked against the number of registered fractures in Boremap. The quality routines include also daily controls of the mapping by detailed examination of Boremap generated variable/summary reports and WellCad log to match. The final quality check of the mapping was done by a routine in the Boremap software. The primary data were subsequently exported to the SKB database SICADA, where they are traceable by the activity plan number.
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4.4 AnalysesandinterpretationsA major flaw in Boremap system is the distinction between fractures that intersect the whole borehole (‘infinite fractures’) and those that end within the drill core (‘finite fractures’). The latter category includes fractures that (1) are slightly curved and runs more or less parallel with the borehole axis, (2) ends in other fractures, (3) splays from other fractures and (4) with no immediately obvious reason ends in the drill core. For modelling purposes, it was decided to separate those fractures that intersect the central borehole axis from those that never reach the centre. Fractures limited to less than half of the borehole are, therefore, marked by ‘#’ in the attached comments.
Another problem with the core logging system is related to geological features (mainly fractures) that can be observed only in the drill core. This problem usually arises from poor resolution in the BIPS-image, which in the present case often is caused by the occurrence of suspension from drilling, brownish black coating from the drilling rods on the borehole walls and/or disturbances in the movement of the BIPS-camera. However, even in the most perfect BIPS-image, it is sometimes difficult to distinguish a thin fracture, sealed by a low contrast mineral. All fractures observed in the drill core, but not recognized in the BIPS-image, have been registered as ‘not visible in BIPS’ in Boremap, to prevent them from being used in forthcoming fracture orientation analysis. If possible, they are still oriented relative to other structures. Fractures supposed to be induced by the drilling activities fall within this category. Obviously drilling-induced fractures are not included in the mapping.
The resolution of the BIPS-image does generally make it possible to estimate the width of fractures with an error of ± 0.5 millimetres. Thus, reliable measurements of fracture widths/apertures less than 1 millimetre are possible to obtain in the drill core, and the minimum width/aperture given is therefore 0.5 millimetre.
The fracture mapping focuses on the division into broken and unbroken fractures, depend-ing on whether they are parting the core or not. Broken fractures include both open fractures and originally sealed fractures, which were broken during the drilling. To decide if a fracture was open, partly open or sealed in the rock volume (i.e. in situ), SKB has developed a confidence classification expressed at three levels, ‘possible’, ‘probable’ and ‘certain’, on the basis of the weathering of the fracture surface and fit of the fracture planes. The criteria for this classification are given in SKB method description for Boremap mapping, SKB MD 143.006 (v 2.0).
Up to four infilling minerals can be registered in the database for each fracture. As far as possible, they are given in order of decreasing abundance in the fracture. Additional miner-als (i.e. five or more), which occur in a few fractures, are noted in the attached comment. However, it must be emphasized that this provides no information of the volumetric amount of individual minerals. In a fracture with two minerals, the mineral registered as ‘second mineral’ may range from sub-microscopic staining up to amounts equal to that of the mineral registered as ‘first mineral’. Hematite, for example, occur consistently as extremely thin coatings or impurities in other fracture minerals, such as adularia and laumontite.
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4.5 NonconformitiesSome fracture filling minerals are more conspicuous than other. For example, the distinct red tinting shown by sub-microscopic hematite reveals extremely low concentrations of the mineral. Also the use of diluted hydrochloric acid for identification of calcite makes it possible to detect amounts that are macroscopically invisible. The amount of fractures filled with other less conspicuous minerals may, on the other hand, be underestimated. Pyrite, which typically forms up to millimetre-sized, isolated crystals, might for example be under-represented in unbroken fractures.
As in previous cored boreholes, the comparative mapping of KFM06C was locally ham-pered by brownish black coatings on the borehole walls as well as mottling of the BIPS-image. The dark coating is frequent in the mapped interval, where it typically forms a spiral pattern or a single band along the borehole axis. This coating phenomenon is obviously drill induced, and the explanation proposed is that the coatings originate from metal frag-ments abraded from the drill rods. Intervals with mottled BIPS-image occur at four levels: 201.64–202.14, 230.58–232.16, 269.25–271.80, 284.45–286.68 metres (adjusted length). Geological features (e.g. fractures) depicted in these mottled intervals are typically distorted and sometimes difficult to distinguish (Figure 4-1). The mottling is obviously a result of disturbances in the normally constant movement of the BIPS-camera.
Figure 4-1. Mottling of the BIPS-image, due to disturbances in the logging movement of the BIPS-camera.
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5 Results
5.1 CorelithologyThe 184.4 metres long interval of KFM06C, which was subjected to the comparative map-ping, is dominated by a medium-grained metagranite (rock code 101057) with a tendency to be slightly granodioritic. Other frequent rock units in the interval includes pegmatitic granite (rock code 101061), amphibolite (rock code 102017), aplitic metagranite (rock code 101058) and fine- to finely medium-grained granite (rock code 111058). The maxi-mum length of individual occurrences is ca 6.8 metres, though the vast majority are less than a few metres in length. Except for some late veins or dykes, all rocks have experienced Svecofennian metamorphism under amphibolite facies conditions.
The medium-grained metagranite (101057) is rather equigranular with elongated quartz domains, alternating with feldspar-dominated domains and thin streaks of biotite. The colour of the rock varieties ranges from greyish red to grey, whereas completely grey varieties, lacking the reddish tint, are sparse and typically associated with amphibolites.
Amphibolites (102017) and related rocks are generally fine-grained, equigranular and with a large proportion of biotite. All extensions and contacts are broadly parallel with the tectonic fabric.
Dykes, veins and segregations of pegmatite, pegmatitic granite, aplite and leucogranitic material are frequent throughout the interval. Most occurrences are some decimetre or less, but several pegmatites/pegmatitic granites reach up to a few metres in length. The pegmatitic granites are generally texturally heterogeneous, often with a highly variable grain-size, and some occurrences include intervals of finely medium-grained, equigranular granite. Rather coarse magnetite, and subordinately hematite, has been identified in some pegmatites. Despite the textural variability and temporal span within this unit, most of these rocks were grouped as ‘pegmatite, pegmatitic granite’ (101061). Other, related rocks, which includes aplitic metagranite (101058), fine- to finely medium-grained granite (111058) and aplite (1062) are often highly reminiscent of each other. A distinctive criterion apart from the late-tectonic character of the aplite (1062) and the fine- to finely medium-grained granite (111058), is the anomalously high natural gamma radiation of fine- to finely medium-grained granite. Quartz-dominated segregations or veins were coded as 8021.
In addition, there are a few minor occurrences of granodiorite and tonalite in the interval. None of them appears to fit into the bedrock nomenclature defined by SKB (‘Regler för bergarters benämningar vid platsundersökningarna i Simpevarp och Forsmark’, v 1.0). Instead they were coded as 1056 (unspecified granodiorite) and 1053 (unspecified tonalite).
5.2 DuctilestructuresMost rocks in the mapped interval of KFM06C are characterised by composite L-S fabrics, with a slight predominance of linear mineral fabrics. However, the relative intensity of the two components is locally variable. The intensity of the deformational fabric is mostly weak to medium. It must, however, be emphasized that it often is difficult to distinguish tectonic fabric visually in the pegmatites and some of the fine-grained mafic rocks. The fact that they may appear massive does not necessarily implicate that they actually are
18
post-kinematic. The foliation is generally E–W trending with a moderate dip towards south. None of the linear fabrics have been possible to register with the present methodology, but the general impression is that they are gently to moderately dipping.
Totally seven narrow zones of more intense ductile deformation have been registered in the mapped interval of KFM06C. All of them are found in a ca 50 metres long interval between 180 and 230 metres (adjusted length). Except for a 1.4 metre wide zone at 223.6–225.0 metres adjusted length, individual zones range up to about three decimetres. The protolith in the zones seems mainly to be a highly deformed and grain-size reduced variety of the metagranite (101057). All shear zones are more or less parallel with the local tectonic foliation.
5.3 AlterationExcept for a decimetre-wide occurrence of pre-metamorphic albitization in the aplitic metagranite (101058), the only alteration encountered in the mapped interval of KFM06C is varying degrees of oxidation, manifested as red pigmentation of feldspars. It is generally associated with more intensely fractured intervals, and is most frequent in the length inter-val 262–297 metres (adjusted length). The oxidation is normally faint to weak in intensity.
5.4 Fractures5.4.1 Fracturefrequenciesandorientations
Excluding crush zones and sealed networks, the total number of open (broken fractures with aperture > 0), partly open (unbroken fractures with aperture > 0) and sealed fractures (broken and unbroken fractures with aperture = 0) registered during the comparative map-ping of KFM06C amounts to 646, i.e. about 3.5 fractures/m. Of these are 483 visible in the BIPS-image. Moreover, they can be separated in 219 open, 14 partly open and 413 sealed fractures. It should be emphasized that there is a certain degree of uncertainty whether a fracture actually is open or sealed. Throughout the borehole, the frequency of open and sealed fractures varies rather coherently, with an increased number of open fractures in intervals with concentrations of sealed fractures (Appendix 1). Considering the fracture distribution along the mapped interval of KFM06C, there is two sections with somewhat increased fracture frequency: 204–228 and 285–305 metres adjusted length. None of these intervals are especially well-defined, and both are dominated by fractures inferred to be sealed.
The fracture orientations vary considerably throughout the mapped interval of KFM06C, though a stereographic projection in Figure 5-1 reveal three rather distinct fracture sets. The proportion of open and sealed fractures differs significantly between the sets. The first fracture set consists of horizontal to sub-horizontal fractures. Fractures of this set are found throughout both borehole, and most of these fractures are inferred to be open. The maximum aperture of these fractures is 4 millimetres. A second fracture set consists steeply dipping fractures, striking N–S. The majority of these fractures are sealed. A third, well-defined fracture set, mainly restricted to the length interval below ca 280 metres, consists of vertical to sub-vertical fractures with ENE–WSW strike. In addition, there are a number of fractures with varying dips towards south. A considerable amount of these fractures are inferred to be open.
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Two rather narrow crush zones occur at 284.66–284.76 and 346.53–346.57 metres (adjusted length) in the mapped interval of KFM06C. Both are gently dipping with an approximate NE–SW trending strike. There is also a drill induced crush in the adjusted length interval 284.66–285.11 metres, which hence overlaps with the upper of the two crush zones.
Five sealed networks with fractures of highly variable orientation have been registered in the mapped interval of KFM06C. The width of individual networks ranges up to a few decimetres.
One fracture inferred to be core discing has been observed at 258.22 metres adjusted length.
5.4.2 Fracturemineralogy
Chlorite and/or calcite are found in about 75% of the total number of the registered fractures in the mapped interval of KFM06C. They are found in all fracture sets discussed above (cf Figure 5-1). Other infilling minerals, in order of decreasing abundance, include clay minerals, prehnite, adularia, pyrite, quartz, laumontite, sub-microscopic hematite, biotite, sericite, epidote, fluorite, galena and unspecified sulphides. There are also 80 fractures that are virtually free from visible mineral coatings and oxidized walls. These are mostly open, and a considerable proportion belongs to the horizontal to sub-horizontal fracture set.
The various clay minerals occur typically in open, flat-lying fractures. It is generally impossible to be more specific regarding the type of clay minerals. However, clay minerals registered in more steeply dipping fractures are mostly corrensite, often intimately associ-ated with chlorite.
Figure 5-1. Lower hemisphere, equal-area stereographic projections showing the poles to all sealed (blue squares) and open (red squares) fractures in the adjusted length interval 176.5–360.9 metres of borehole KFM06C. A filled, black circle mark the orientation of the borehole axis.
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All other minerals, as well as the presence of oxidized walls, are preferentially associated with sealed fractures. A typical mineral assemblage is calcite + chlorite ± hematite stained adularia ± pyrite. The assemblage is found in all the fracture sets discussed above, though the third fracture set is dominated by hematite-stained adularia with subordinate amounts of calcite and chlorite. Laumontite and to some extent quartz tend to be associated with this assemblage. Fractures containing this assemblage often exhibit oxidized walls. A number of very thin (<< 1 millimetre), sealed fractures are only revealed by their oxidized walls. Except for staining of various silicates, such as adularia and laumontite, hematite may occur as thin, reddish coatings, preferentially found in flat lying fractures.
Prehnite is more or less restricted to sealed fractures in amphibolites. Most of these fractures are rather thin (< 1 millimetre). The identification is therefore difficult and some of the light greenish mineral mapped as prehnite might be adularia or possibly epidote.
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Dateofcoremapping
CoordinateSystem RT90-RHB70
Length[m]
Title GEOLOGYINKFM06C
Diameter[mm] 77.0Elevation[m.a.s.l.]
Borehole KFM06C
Inclination[°] -60.0
Site FORSMARKNorthing[m]Easting[m]
Fracturedatafrom
Appendix: 1
DrillingStopDatePlotDate
Bearing[°] 26.1
Rocktypedatafrom
DrillingStartDate
1:500
DEP
TH.
TYP
E
Stru
ctur
e
Text
ure
Gra
insi
ze
Stru
ctur
eO
rient
atio
n
Roc
k Ty
pe<
1m
Alte
ratio
n
Inte
nsity
ROCKTYPE
Prim
ary
Min
eral
Sec
onda
ryM
iner
al
Third
Min
eral
Four
thM
iner
al
Alte
ratio
nO
rient
atio
n
SEALEDFRACTURES
Prim
ary
Min
eral
Sec
onda
ryM
iner
al
Third
Min
eral
Four
thM
iner
al
Rou
ghne
ss
Sur
face
Alte
ratio
nO
rient
atio
n
Ape
rture
(mm
)
NATURAL FRACTURES
Alte
ratio
n
Pie
ce
Cor
elos
s
CRUSHZONE
Frequency (fr/m)
0 20
FRACTURE
180
190
200
210
220
230
240
250
260
270
280
290
10.0
Page 1
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Appendix2
BoreholediametersHoleDiamT–Drilling:BoreholediameterKFM06C,2005‑04‑2714:30:00–2005‑06‑3013:44:00(100.400–1,000.430m).
Subsecup(m)
Subseclow(m)
Holediam(m)
Comment
100.400 102.080 0.086102.080 1,000.430 0.077
Printout from SICADA 2005-10-12 16:50:52.
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App
endi
x3
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nhol
ede
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ion
mea
sure
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tsM
axib
orT
–B
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ole
devi
atio
n:M
axib
orK
FM06
C,2
005‑
08‑0
211
:01:
00–
200
5‑08
‑02
20:1
9:00
(3.0
00–9
78.0
00m
).
Leng
th
(m)
Nor
thin
g(m
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stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
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calB
(m
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(m
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olfl
ag
3.00
6699
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3243
7.69
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.86
1.49
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6699
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0.03
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–59.
8726
.65
7.49
000.
0000
0.02
0021
.00
6699
750.
3816
3244
1.66
14.1
1R
T90-
RH
B70
–59.
8226
.71
9.00
000.
0200
0.03
0024
.00
6699
751.
7216
3244
2.33
16.7
0R
T90-
RH
B70
–59.
7526
.71
10.5
000
0.04
000.
0500
27.0
066
9975
3.07
1632
443.
0119
.29
RT9
0-R
HB
70–5
9.67
26.8
212
.010
00.
0500
0.07
0030
.00
6699
754.
4216
3244
3.70
21.8
8R
T90-
RH
B70
–59.
6127
.06
13.5
300
0.07
000.
0900
33.0
066
9975
5.78
1632
444.
3924
.47
RT9
0-R
HB
70–5
9.56
27.1
915
.050
00.
1000
0.12
0036
.00
6699
757.
1316
3244
5.08
27.0
6R
T90-
RH
B70
–59.
5427
.24
16.5
700
0.13
000.
1500
39.0
066
9975
8.48
1632
445.
7829
.64
RT9
0-R
HB
70–5
9.49
27.2
318
.090
00.
1600
0.18
0042
.00
6699
759.
8316
3244
6.47
32.2
3R
T90-
RH
B70
–59.
4327
.21
19.6
100
0.19
000.
2100
45.0
066
9976
1.19
1632
447.
1734
.81
RT9
0-R
HB
70–5
9.42
27.2
021
.140
00.
2200
0.25
0048
.00
6699
762.
5516
3244
7.87
37.3
9R
T90-
RH
B70
–59.
3527
.21
22.6
600
0.25
000.
2800
51.0
066
9976
3.91
1632
448.
5739
.97
RT9
0-R
HB
70–5
9.25
27.3
324
.190
00.
2800
0.32
0054
.00
6699
765.
2716
3244
9.27
42.5
5R
T90-
RH
B70
–59.
1027
.42
25.7
200
0.32
000.
3700
57.0
066
9976
6.64
1632
449.
9845
.12
RT9
0-R
HB
70–5
8.97
27.5
227
.260
00.
3500
0.42
0060
.00
6699
768.
0116
3245
0.70
47.7
0R
T90-
RH
B70
–58.
7927
.44
28.8
100
0.39
000.
4800
28
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
63.0
066
9976
9.39
1632
451.
4150
.26
RT9
0-R
HB
70–5
8.58
27.2
930
.360
00.
4300
0.55
0066
.00
6699
770.
7816
3245
2.13
52.8
2R
T90-
RH
B70
–58.
4927
.30
31.9
300
0.46
000.
6300
69.0
066
9977
2.17
1632
452.
8555
.38
RT9
0-R
HB
70–5
8.46
27.4
133
.500
00.
5000
0.71
0072
.00
6699
773.
5716
3245
3.57
57.9
4R
T90-
RH
B70
–58.
4127
.49
35.0
600
0.53
000.
8000
75.0
066
9977
4.96
1632
454.
3060
.49
RT9
0-R
HB
70–5
8.30
27.5
836
.640
00.
5700
0.89
0078
.00
6699
776.
3616
3245
5.03
63.0
4R
T90-
RH
B70
–58.
2227
.62
38.2
100
0.61
000.
9800
81.0
066
9977
7.76
1632
455.
7665
.59
RT9
0-R
HB
70–5
8.30
27.5
139
.790
00.
6600
1.08
0084
.00
6699
779.
1616
3245
6.49
68.1
5R
T90-
RH
B70
–58.
2827
.25
41.3
700
0.70
001.
1800
87.0
066
9978
0.56
1632
457.
2170
.70
RT9
0-R
HB
70–5
8.19
27.1
342
.940
00.
7300
1.27
0090
.00
6699
781.
9716
3245
7.93
73.2
5R
T90-
RH
B70
–58.
1527
.21
44.5
200
0.76
001.
3800
93.0
066
9978
3.37
1632
458.
6675
.80
RT9
0-R
HB
70–5
8.05
27.2
446
.110
00.
7900
1.48
0096
.00
6699
784.
7916
3245
9.38
78.3
4R
T90-
RH
B70
–58.
0127
.23
47.6
900
0.82
001.
5900
99.0
066
9978
6.20
1632
460.
1180
.89
RT9
0-R
HB
70–5
8.24
27.0
449
.280
00.
8600
1.70
0010
2.00
6699
787.
6116
3246
0.83
83.4
4R
T90-
RH
B70
–58.
5626
.73
50.8
600
0.88
001.
8000
105.
0066
9978
9.00
1632
461.
5386
.00
RT9
0-R
HB
70–5
8.53
26.7
152
.430
00.
9000
1.88
0010
8.00
6699
790.
4016
3246
2.23
88.5
6R
T90-
RH
B70
–58.
4326
.94
53.9
900
0.92
001.
9600
111.
0066
9979
1.80
1632
462.
9591
.11
RT9
0-R
HB
70–5
8.36
27.1
855
.560
00.
9400
2.05
0011
4.00
6699
793.
2016
3246
3.67
93.6
7R
T90-
RH
B70
–58.
3427
.31
57.1
400
0.97
002.
1400
117.
0066
9979
4.60
1632
464.
3996
.22
RT9
0-R
HB
70–5
8.31
27.3
658
.710
01.
0100
2.23
0012
0.00
6699
796.
0016
3246
5.11
98.7
7R
T90-
RH
B70
–58.
2227
.44
60.2
900
1.04
002.
3300
123.
0066
9979
7.40
1632
465.
8410
1.32
RT9
0-R
HB
70–5
8.12
27.6
361
.870
01.
0800
2.43
0012
6.00
6699
798.
8116
3246
6.58
103.
87R
T90-
RH
B70
–58.
0027
.83
63.4
500
1.13
002.
5300
129.
0066
9980
0.21
1632
467.
3210
6.41
RT9
0-R
HB
70–5
7.90
28.0
265
.040
01.
1700
2.64
0013
2.00
6699
801.
6216
3246
8.07
108.
95R
T90-
RH
B70
–57.
7528
.17
66.6
300
1.23
002.
7600
135.
0066
9980
3.03
1632
468.
8211
1.49
RT9
0-R
HB
70–5
7.63
28.3
768
.230
01.
2900
2.88
0013
8.00
6699
804.
4416
3246
9.59
114.
03R
T90-
RH
B70
–57.
5228
.62
69.8
400
1.35
003.
0100
141.
0066
9980
5.86
1632
470.
3611
6.56
RT9
0-R
HB
70–5
7.42
28.8
571
.450
01.
4200
3.14
0014
4.00
6699
807.
2716
3247
1.14
119.
08R
T90-
RH
B70
–57.
3329
.09
73.0
600
1.50
003.
2800
2�
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
147.
0066
9980
8.69
1632
471.
9212
1.61
RT9
0-R
HB
70–5
7.26
29.3
374
.680
01.
5900
3.43
0015
0.00
6699
810.
1016
3247
2.72
124.
13R
T90-
RH
B70
–57.
1829
.60
76.3
000
1.68
003.
5800
153.
0066
9981
1.52
1632
473.
5212
6.65
RT9
0-R
HB
70–5
7.14
29.8
377
.920
01.
7800
3.73
0015
6.00
6699
812.
9316
3247
4.33
129.
17R
T90-
RH
B70
–57.
1230
.06
79.5
500
1.89
003.
8800
159.
0066
9981
4.34
1632
475.
1513
1.69
RT9
0-R
HB
70–5
7.07
30.2
481
.170
02.
0000
4.03
0016
2.00
6699
815.
7516
3247
5.97
134.
21R
T90-
RH
B70
–57.
0230
.33
82.8
000
2.12
004.
1900
165.
0066
9981
7.16
1632
476.
7913
6.73
RT9
0-R
HB
70–5
6.97
30.4
084
.430
02.
2400
4.35
0016
8.00
6699
818.
5716
3247
7.62
139.
24R
T90-
RH
B70
–56.
9030
.47
86.0
600
2.36
004.
5100
171.
0066
9981
9.98
1632
478.
4514
1.76
RT9
0-R
HB
70–5
6.80
30.6
787
.690
02.
4900
4.67
0017
4.00
6699
821.
3916
3247
9.29
144.
27R
T90-
RH
B70
–56.
6930
.83
89.3
300
2.62
004.
8400
177.
0066
9982
2.81
1632
480.
1314
6.77
RT9
0-R
HB
70–5
6.61
31.0
390
.970
02.
7600
5.02
0018
0.00
6699
824.
2216
3248
0.98
149.
28R
T90-
RH
B70
–56.
5331
.23
92.6
100
2.90
005.
1900
183.
0066
9982
5.64
1632
481.
8415
1.78
RT9
0-R
HB
70–5
6.45
31.4
594
.260
03.
0500
5.38
0018
6.00
6699
827.
0516
3248
2.71
154.
28R
T90-
RH
B70
–56.
3731
.68
95.9
100
3.21
005.
5600
189.
0066
9982
8.47
1632
483.
5815
6.78
RT9
0-R
HB
70–5
6.31
31.8
897
.570
03.
3700
5.75
0019
2.00
6699
829.
8816
3248
4.46
159.
28R
T90-
RH
B70
–56.
2732
.11
99.2
200
3.54
005.
9400
195.
0066
9983
1.29
1632
485.
3416
1.77
RT9
0-R
HB
70–5
6.19
32.3
410
0.88
003.
7100
6.14
0019
8.00
6699
832.
7016
3248
6.24
164.
26R
T90-
RH
B70
–56.
1032
.55
102.
5400
3.90
006.
3300
201.
0066
9983
4.11
1632
487.
1416
6.75
RT9
0-R
HB
70–5
5.98
32.7
910
4.20
004.
0900
6.53
0020
4.00
6699
835.
5216
3248
8.05
169.
24R
T90-
RH
B70
–55.
8433
.00
105.
8700
4.28
006.
7400
207.
0066
9983
6.93
1632
488.
9617
1.72
RT9
0-R
HB
70–5
5.74
33.2
110
7.54
004.
4900
6.95
0021
0.00
6699
838.
3516
3248
9.89
174.
20R
T90-
RH
B70
–55.
6333
.44
109.
2100
4.70
007.
1700
213.
0066
9983
9.76
1632
490.
8217
6.68
RT9
0-R
HB
70–5
5.56
33.5
811
0.89
004.
9100
7.40
0021
6.00
6699
841.
1716
3249
1.76
179.
15R
T90-
RH
B70
–55.
5433
.75
112.
5800
5.13
007.
6200
219.
0066
9984
2.59
1632
492.
7018
1.62
RT9
0-R
HB
70–5
5.53
33.9
711
4.26
005.
3600
7.85
0022
2.00
6699
843.
9916
3249
3.65
184.
10R
T90-
RH
B70
–55.
5234
.18
115.
9400
5.60
008.
0700
225.
0066
9984
5.40
1632
494.
6118
6.57
RT9
0-R
HB
70–5
5.50
34.4
311
7.62
005.
8400
8.30
0022
8.00
6699
846.
8016
3249
5.57
189.
04R
T90-
RH
B70
–55.
4834
.66
119.
3000
6.08
008.
5300
�0
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
231.
0066
9984
8.20
1632
496.
5319
1.52
RT9
0-R
HB
70–5
5.45
34.8
812
0.98
006.
3400
8.75
0023
4.00
6699
849.
5916
3249
7.51
193.
99R
T90-
RH
B70
–55.
4135
.09
122.
6600
6.60
008.
9800
237.
0066
9985
0.99
1632
498.
4919
6.46
RT9
0-R
HB
70–5
5.37
35.2
712
4.35
006.
8600
9.21
0024
0.00
6699
852.
3816
3249
9.47
198.
92R
T90-
RH
B70
–55.
3235
.43
126.
0300
7.14
009.
4400
243.
0066
9985
3.77
1632
500.
4620
1.39
RT9
0-R
HB
70–5
5.28
35.6
112
7.71
007.
4200
9.67
0024
6.00
6699
855.
1616
3250
1.46
203.
86R
T90-
RH
B70
–55.
2335
.79
129.
4000
7.70
009.
9000
249.
0066
9985
6.55
1632
502.
4620
6.32
RT9
0-R
HB
70–5
5.20
35.9
613
1.08
007.
9900
10.1
300
252.
0066
9985
7.93
1632
503.
4620
8.78
RT9
0-R
HB
70–5
5.17
36.1
513
2.77
008.
2800
10.3
700
255.
0066
9985
9.32
1632
504.
4721
1.25
RT9
0-R
HB
70–5
5.14
36.3
613
4.46
008.
5800
10.6
100
258.
0066
9986
0.70
1632
505.
4921
3.71
RT9
0-R
HB
70–5
5.10
36.5
813
6.15
008.
8900
10.8
400
261.
0066
9986
2.08
1632
506.
5121
6.17
RT9
0-R
HB
70–5
5.08
36.7
713
7.83
009.
2000
11.0
800
264.
0066
9986
3.45
1632
507.
5421
8.63
RT9
0-R
HB
70–5
5.05
36.9
713
9.52
009.
5200
11.3
200
267.
0066
9986
4.83
1632
508.
5722
1.09
RT9
0-R
HB
70–5
5.00
37.1
414
1.21
009.
8500
11.5
600
270.
0066
9986
6.20
1632
509.
6122
3.55
RT9
0-R
HB
70–5
4.92
37.2
614
2.90
0010
.180
011
.800
027
3.00
6699
867.
5716
3251
0.66
226.
00R
T90-
RH
B70
–54.
8637
.38
144.
5900
10.5
100
12.0
400
276.
0066
9986
8.94
1632
511.
7022
8.45
RT9
0-R
HB
70–5
4.84
37.4
814
6.28
0010
.850
012
.280
027
9.00
6699
870.
3116
3251
2.76
230.
91R
T90-
RH
B70
–54.
8637
.57
147.
9700
11.1
900
12.5
300
282.
0066
9987
1.68
1632
513.
8123
3.36
RT9
0-R
HB
70–5
4.86
37.7
514
9.67
0011
.540
012
.780
028
5.00
6699
873.
0516
3251
4.87
235.
81R
T90-
RH
B70
–54.
8337
.86
151.
3600
11.8
900
13.0
200
288.
0066
9987
4.41
1632
515.
9323
8.27
RT9
0-R
HB
70–5
4.77
37.9
915
3.05
0012
.240
013
.260
029
1.00
6699
875.
7716
3251
6.99
240.
72R
T90-
RH
B70
–54.
7238
.17
154.
7400
12.6
000
13.5
100
294.
0066
9987
7.14
1632
518.
0624
3.17
RT9
0-R
HB
70–5
4.66
38.3
915
6.44
0012
.960
013
.760
029
7.00
6699
878.
5016
3251
9.14
245.
61R
T90-
RH
B70
–54.
5838
.63
158.
1300
13.3
300
14.0
100
300.
0066
9987
9.85
1632
520.
2324
8.06
RT9
0-R
HB
70–5
4.51
38.8
815
9.83
0013
.710
014
.270
030
3.00
6699
881.
2116
3252
1.32
250.
50R
T90-
RH
B70
–54.
4339
.08
161.
5300
14.1
000
14.5
200
306.
0066
9988
2.57
1632
522.
4225
2.94
RT9
0-R
HB
70–5
4.34
39.2
416
3.23
0014
.490
014
.780
030
9.00
6699
883.
9216
3252
3.52
255.
38R
T90-
RH
B70
–54.
2439
.44
164.
9300
14.8
900
15.0
400
312.
0066
9988
5.27
1632
524.
6425
7.81
RT9
0-R
HB
70–5
4.13
39.6
816
6.64
0015
.290
015
.310
0
�1
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
315.
0066
9988
6.63
1632
525.
7626
0.24
RT9
0-R
HB
70–5
4.05
39.9
316
8.34
0015
.710
015
.580
031
8.00
6699
887.
9816
3252
6.89
262.
67R
T90-
RH
B70
–53.
9640
.19
170.
0500
16.1
300
15.8
500
321.
0066
9988
9.33
1632
528.
0326
5.10
RT9
0-R
HB
70–5
3.86
40.3
717
1.77
0016
.560
016
.130
032
4.00
6699
890.
6716
3252
9.18
267.
52R
T90-
RH
B70
–53.
8240
.49
173.
4800
17.0
000
16.4
100
327.
0066
9989
2.02
1632
530.
3326
9.94
RT9
0-R
HB
70–5
3.75
40.6
917
5.20
0017
.440
016
.690
033
0.00
6699
893.
3716
3253
1.48
272.
36R
T90-
RH
B70
–53.
6640
.89
176.
9100
17.8
900
16.9
700
333.
0066
9989
4.71
1632
532.
6527
4.78
RT9
0-R
HB
70–5
3.56
41.0
517
8.63
0018
.340
017
.260
033
6.00
6699
896.
0516
3253
3.82
277.
19R
T90-
RH
B70
–53.
4541
.24
180.
3500
18.8
000
17.5
500
339.
0066
9989
7.40
1632
534.
9927
9.60
RT9
0-R
HB
70–5
3.34
41.4
018
2.08
0019
.270
017
.840
034
2.00
6699
898.
7416
3253
6.18
282.
01R
T90-
RH
B70
–53.
2441
.48
183.
8000
19.7
400
18.1
400
345.
0066
9990
0.08
1632
537.
3728
4.41
RT9
0-R
HB
70–5
3.16
41.5
718
5.53
0020
.220
018
.440
034
8.00
6699
901.
4316
3253
8.56
286.
81R
T90-
RH
B70
–53.
0941
.76
187.
2700
20.7
000
18.7
500
351.
0066
9990
2.77
1632
539.
7628
9.21
RT9
0-R
HB
70–5
3.04
41.9
418
9.00
0021
.190
019
.060
035
4.00
6699
904.
1216
3254
0.97
291.
61R
T90-
RH
B70
–52.
9942
.14
190.
7400
21.6
800
19.3
700
357.
0066
9990
5.46
1632
542.
1829
4.00
RT9
0-R
HB
70–5
2.94
42.3
719
2.47
0022
.180
019
.680
036
0.00
6699
906.
7916
3254
3.40
296.
40R
T90-
RH
B70
–52.
9142
.62
194.
2100
22.6
900
19.9
900
363.
0066
9990
8.12
1632
544.
6229
8.79
RT9
0-R
HB
70–5
2.87
42.8
619
5.94
0023
.210
020
.300
036
6.00
6699
909.
4516
3254
5.85
301.
18R
T90-
RH
B70
–52.
8143
.10
197.
6800
23.7
300
20.6
100
369.
0066
9991
0.77
1632
547.
0930
3.57
RT9
0-R
HB
70–5
2.76
43.2
819
9.41
0024
.260
020
.930
037
2.00
6699
912.
1016
3254
8.34
305.
96R
T90-
RH
B70
–52.
7043
.48
201.
1400
24.8
000
21.2
400
375.
0066
9991
3.42
1632
549.
5930
8.35
RT9
0-R
HB
70–5
2.64
43.6
820
2.88
0025
.340
021
.560
037
8.00
6699
914.
7316
3255
0.85
310.
73R
T90-
RH
B70
–52.
6043
.89
204.
6100
25.8
900
21.8
700
381.
0066
9991
6.04
1632
552.
1131
3.12
RT9
0-R
HB
70–5
2.55
44.1
220
6.35
0026
.450
022
.190
038
4.00
6699
917.
3516
3255
3.38
315.
50R
T90-
RH
B70
–52.
5044
.32
208.
0800
27.0
100
22.5
100
387.
0066
9991
8.66
1632
554.
6531
7.88
RT9
0-R
HB
70–5
2.48
44.5
420
9.82
0027
.590
022
.820
039
0.00
6699
919.
9616
3255
5.94
320.
26R
T90-
RH
B70
–52.
4244
.82
211.
5500
28.1
700
23.1
400
393.
0066
9992
1.26
1632
557.
2332
2.63
RT9
0-R
HB
70–5
2.35
45.0
921
3.28
0028
.750
023
.460
039
6.00
6699
922.
5516
3255
8.52
325.
01R
T90-
RH
B70
–52.
2645
.31
215.
0100
29.3
500
23.7
800
�2
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
399.
0066
9992
3.85
1632
559.
8332
7.38
RT9
0-R
HB
70–5
2.12
45.4
821
6.75
0029
.960
024
.100
040
2.00
6699
925.
1416
3256
1.14
329.
75R
T90-
RH
B70
–52.
0045
.64
218.
4800
30.5
700
24.4
300
405.
0066
9992
6.43
1632
562.
4633
2.11
RT9
0-R
HB
70–5
1.89
45.8
122
0.22
0031
.190
024
.760
040
8.00
6699
927.
7216
3256
3.79
334.
47R
T90-
RH
B70
–51.
8046
.02
221.
9700
31.8
100
25.0
900
411.
0066
9992
9.01
1632
565.
1333
6.83
RT9
0-R
HB
70–5
1.72
46.2
122
3.71
0032
.450
025
.430
041
4.00
6699
930.
2916
3256
6.47
339.
19R
T90-
RH
B70
–51.
6446
.39
225.
4600
33.0
900
25.7
700
417.
0066
9993
1.58
1632
567.
8234
1.54
RT9
0-R
HB
70–5
1.58
46.5
722
7.20
0033
.730
026
.110
042
0.00
6699
932.
8616
3256
9.17
343.
89R
T90-
RH
B70
–51.
5246
.74
228.
9500
34.3
900
26.4
500
423.
0066
9993
4.14
1632
570.
5334
6.24
RT9
0-R
HB
70–5
1.47
46.9
023
0.69
0035
.050
026
.800
042
6.00
6699
935.
4216
3257
1.89
348.
58R
T90-
RH
B70
–51.
4547
.05
232.
4400
35.7
100
27.1
400
429.
0066
9993
6.69
1632
573.
2635
0.93
RT9
0-R
HB
70–5
1.39
47.1
923
4.19
0036
.380
027
.490
043
2.00
6699
937.
9616
3257
4.63
353.
28R
T90-
RH
B70
–51.
2747
.37
235.
9300
37.0
600
27.8
300
435.
0066
9993
9.23
1632
576.
0235
5.62
RT9
0-R
HB
70–5
1.20
47.5
723
7.68
0037
.740
028
.180
043
8.00
6699
940.
5016
3257
7.40
357.
95R
T90-
RH
B70
–51.
1547
.81
239.
4300
38.4
300
28.5
400
441.
0066
9994
1.77
1632
578.
8036
0.29
RT9
0-R
HB
70–5
1.14
48.0
124
1.18
0039
.120
028
.890
044
4.00
6699
943.
0216
3258
0.20
362.
63R
T90-
RH
B70
–51.
1148
.23
242.
9200
39.8
300
29.2
400
447.
0066
9994
4.28
1632
581.
6036
4.96
RT9
0-R
HB
70–5
1.02
48.4
024
4.67
0040
.540
029
.590
045
0.00
6699
945.
5316
3258
3.01
367.
29R
T90-
RH
B70
–50.
9548
.56
246.
4100
41.2
500
29.9
400
453.
0066
9994
6.78
1632
584.
4336
9.62
RT9
0-R
HB
70–5
0.87
48.7
724
8.16
0041
.980
030
.290
045
6.00
6699
948.
0316
3258
5.85
371.
95R
T90-
RH
B70
–50.
8048
.96
249.
9100
42.7
100
30.6
500
459.
0066
9994
9.28
1632
587.
2837
4.27
RT9
0-R
HB
70–5
0.72
49.2
025
1.65
0043
.450
031
.000
046
2.00
6699
950.
5216
3258
8.72
376.
60R
T90-
RH
B70
–50.
6549
.43
253.
4000
44.1
900
31.3
600
465.
0066
9995
1.75
1632
590.
1737
8.92
RT9
0-R
HB
70–5
0.64
49.6
425
5.15
0044
.950
031
.720
046
8.00
6699
952.
9916
3259
1.62
381.
24R
T90-
RH
B70
–50.
6449
.82
256.
8900
45.7
100
32.0
800
471.
0066
9995
4.21
1632
593.
0738
3.56
RT9
0-R
HB
70–5
0.65
50.0
025
8.63
0046
.470
032
.430
047
4.00
6699
955.
4416
3259
4.53
385.
88R
T90-
RH
B70
–50.
6550
.21
260.
3700
47.2
500
32.7
800
477.
0066
9995
6.65
1632
595.
9938
8.20
RT9
0-R
HB
70–5
0.61
50.4
426
2.11
0048
.020
033
.130
048
0.00
6699
957.
8716
3259
7.46
390.
51R
T90-
RH
B70
–50.
5950
.64
263.
8400
48.8
100
33.4
800
��
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
483.
0066
9995
9.07
1632
598.
9339
2.83
RT9
0-R
HB
70–5
0.55
50.8
726
5.57
0049
.600
033
.830
048
6.00
6699
960.
2816
3260
0.41
395.
15R
T90-
RH
B70
–50.
5351
.05
267.
3000
50.4
000
34.1
700
489.
0066
9996
1.48
1632
601.
8939
7.46
RT9
0-R
HB
70–5
0.49
51.2
726
9.03
0051
.210
034
.520
049
2.00
6699
962.
6716
3260
3.38
399.
78R
T90-
RH
B70
–50.
4651
.46
270.
7600
52.0
200
34.8
600
495.
0066
9996
3.86
1632
604.
8740
2.09
RT9
0-R
HB
70–5
0.42
51.6
427
2.48
0052
.840
035
.210
049
8.00
6699
965.
0516
3260
6.37
404.
40R
T90-
RH
B70
–50.
3951
.80
274.
2100
53.6
700
35.5
500
501.
0066
9996
6.23
1632
607.
8840
6.72
RT9
0-R
HB
70–5
0.37
51.9
827
5.93
0054
.500
035
.890
050
4.00
6699
967.
4116
3260
9.38
409.
03R
T90-
RH
B70
–50.
3552
.16
277.
6500
55.3
300
36.2
300
507.
0066
9996
8.58
1632
610.
8941
1.34
RT9
0-R
HB
70–5
0.34
52.3
627
9.37
0056
.170
036
.570
051
0.00
6699
969.
7516
3261
2.41
413.
65R
T90-
RH
B70
–50.
3152
.56
281.
0900
57.0
200
36.9
100
513.
0066
9997
0.92
1632
613.
9341
5.95
RT9
0-R
HB
70–5
0.30
52.7
528
2.80
0057
.880
037
.250
051
6.00
6699
972.
0816
3261
5.46
418.
26R
T90-
RH
B70
–50.
2852
.99
284.
5100
58.7
400
37.5
800
519.
0066
9997
3.23
1632
616.
9942
0.57
RT9
0-R
HB
70–5
0.24
53.2
528
6.22
0059
.610
037
.910
052
2.00
6699
974.
3816
3261
8.53
422.
88R
T90-
RH
B70
–50.
1653
.50
287.
9300
60.4
800
38.2
500
525.
0066
9997
5.52
1632
620.
0742
5.18
RT9
0-R
HB
70–5
0.10
53.7
528
9.63
0061
.370
038
.580
052
8.00
6699
976.
6616
3262
1.62
427.
48R
T90-
RH
B70
–50.
0753
.99
291.
3400
62.2
600
38.9
100
531.
0066
9997
7.79
1632
623.
1842
9.78
RT9
0-R
HB
70–5
0.06
54.2
229
3.04
0063
.160
039
.240
053
4.00
6699
978.
9216
3262
4.74
432.
08R
T90-
RH
B70
–50.
0454
.44
294.
7400
64.0
700
39.5
600
537.
0066
9998
0.04
1632
626.
3143
4.38
RT9
0-R
HB
70–5
0.00
54.6
429
6.43
0064
.990
039
.890
054
0.00
6699
981.
1516
3262
7.88
436.
68R
T90-
RH
B70
–49.
9454
.82
298.
1300
65.9
100
40.2
100
543.
0066
9998
2.27
1632
629.
4643
8.98
RT9
0-R
HB
70–4
9.91
55.0
229
9.82
0066
.840
040
.540
054
6.00
6699
983.
3716
3263
1.04
441.
27R
T90-
RH
B70
–49.
8755
.20
301.
5100
67.7
800
40.8
600
549.
0066
9998
4.48
1632
632.
6344
3.56
RT9
0-R
HB
70–4
9.84
55.4
230
3.20
0068
.720
041
.180
055
2.00
6699
985.
5716
3263
4.22
445.
86R
T90-
RH
B70
–49.
8355
.60
304.
8900
69.6
700
41.5
000
555.
0066
9998
6.67
1632
635.
8244
8.15
RT9
0-R
HB
70–4
9.82
55.7
930
6.57
0070
.620
041
.820
055
8.00
6699
987.
7616
3263
7.42
450.
44R
T90-
RH
B70
–49.
8155
.95
308.
2500
71.5
800
42.1
300
561.
0066
9998
8.84
1632
639.
0345
2.73
RT9
0-R
HB
70–4
9.79
56.1
030
9.93
0072
.540
042
.450
056
4.00
6699
989.
9216
3264
0.63
455.
02R
T90-
RH
B70
–49.
7756
.25
311.
6100
73.5
100
42.7
600
��
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
567.
0066
9999
1.00
1632
642.
2445
7.31
RT9
0-R
HB
70–4
9.72
56.3
931
3.28
0074
.490
043
.070
057
0.00
6699
992.
0716
3264
3.86
459.
60R
T90-
RH
B70
–49.
6356
.52
314.
9500
75.4
700
43.3
800
573.
0066
9999
3.14
1632
645.
4846
1.89
RT9
0-R
HB
70–4
9.56
56.7
031
6.63
0076
.450
043
.690
057
6.00
6699
994.
2116
3264
7.11
464.
17R
T90-
RH
B70
–49.
4756
.87
318.
3000
77.4
400
44.0
100
579.
0066
9999
5.28
1632
648.
7446
6.45
RT9
0-R
HB
70–4
9.36
57.0
531
9.98
0078
.440
044
.330
058
2.00
6699
996.
3416
3265
0.38
468.
73R
T90-
RH
B70
–49.
2557
.23
321.
6500
79.4
500
44.6
400
585.
0066
9999
7.40
1632
652.
0347
1.00
RT9
0-R
HB
70–4
9.18
57.4
132
3.33
0080
.460
044
.960
058
8.00
6699
998.
4516
3265
3.68
473.
27R
T90-
RH
B70
–49.
1557
.62
325.
0000
81.4
800
45.2
800
591.
0066
9999
9.51
1632
655.
3447
5.54
RT9
0-R
HB
70–4
9.12
57.8
132
6.68
0082
.510
045
.600
059
4.00
6700
000.
5516
3265
7.00
477.
81R
T90-
RH
B70
–49.
0957
.95
328.
3500
83.5
400
45.9
200
597.
0067
0000
1.59
1632
658.
6648
0.08
RT9
0-R
HB
70–4
9.05
58.0
433
0.01
0084
.580
046
.240
060
0.00
6700
002.
6316
3266
0.33
482.
34R
T90-
RH
B70
–49.
0258
.14
331.
6800
85.6
200
46.5
600
603.
0067
0000
3.67
1632
662.
0048
4.61
RT9
0-R
HB
70–4
8.96
58.2
833
3.35
0086
.670
046
.870
060
6.00
6700
004.
7116
3266
3.68
486.
87R
T90-
RH
B70
–48.
9158
.41
335.
0100
87.7
200
47.1
900
609.
0067
0000
5.74
1632
665.
3648
9.13
RT9
0-R
HB
70–4
8.88
58.5
633
6.68
0088
.770
047
.510
061
2.00
6700
006.
7716
3266
7.04
491.
39R
T90-
RH
B70
–48.
8458
.71
338.
3400
89.8
300
47.8
300
615.
0067
0000
7.80
1632
668.
7349
3.65
RT9
0-R
HB
70–4
8.79
58.8
534
0.01
0090
.900
048
.140
061
8.00
6700
008.
8216
3267
0.42
495.
91R
T90-
RH
B70
–48.
7458
.94
341.
6700
91.9
700
48.4
600
621.
0067
0000
9.84
1632
672.
1149
8.16
RT9
0-R
HB
70–4
8.68
59.0
234
3.33
0093
.040
048
.780
062
4.00
6700
010.
8616
3267
3.81
500.
41R
T90-
RH
B70
–48.
6459
.08
344.
9900
94.1
200
49.0
900
627.
0067
0001
1.88
1632
675.
5150
2.67
RT9
0-R
HB
70–4
8.61
59.1
734
6.65
0095
.200
049
.410
063
0.00
6700
012.
8916
3267
7.22
504.
92R
T90-
RH
B70
–48.
5759
.31
348.
3200
96.2
800
49.7
300
633.
0067
0001
3.91
1632
678.
9250
7.17
RT9
0-R
HB
70–4
8.52
59.4
734
9.98
0097
.370
050
.050
063
6.00
6700
014.
9216
3268
0.64
509.
41R
T90-
RH
B70
–48.
4759
.61
351.
6400
98.4
600
50.3
700
639.
0067
0001
5.92
1632
682.
3551
1.66
RT9
0-R
HB
70–4
8.42
59.7
935
3.29
0099
.560
050
.690
064
2.00
6700
016.
9216
3268
4.07
513.
90R
T90-
RH
B70
–48.
3759
.93
354.
9500
100.
6700
51.0
100
645.
0067
0001
7.92
1632
685.
8051
6.15
RT9
0-R
HB
70–4
8.32
60.0
435
6.60
0010
1.78
0051
.330
064
8.00
6700
018.
9216
3268
7.52
518.
39R
T90-
RH
B70
–48.
2860
.13
358.
2600
102.
8900
51.6
400
��
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
651.
0067
0001
9.91
1632
689.
2652
0.63
RT9
0-R
HB
70–4
8.27
60.2
635
9.91
0010
4.01
0051
.960
065
4.00
6700
020.
9016
3269
0.99
522.
86R
T90-
RH
B70
–48.
2560
.42
361.
5600
105.
1300
52.2
800
657.
0067
0002
1.89
1632
692.
7352
5.10
RT9
0-R
HB
70–4
8.22
60.5
636
3.21
0010
6.26
0052
.590
066
0.00
6700
022.
8716
3269
4.47
527.
34R
T90-
RH
B70
–48.
1860
.68
364.
8600
107.
3900
52.9
100
663.
0067
0002
3.85
1632
696.
2152
9.58
RT9
0-R
HB
70–4
8.14
60.8
136
6.51
0010
8.53
0053
.220
066
6.00
6700
024.
8316
3269
7.96
531.
81R
T90-
RH
B70
–48.
1260
.95
368.
1500
109.
6700
53.5
300
669.
0067
0002
5.80
1632
699.
7153
4.04
RT9
0-R
HB
70–4
8.11
61.0
936
9.79
0011
0.82
0053
.850
067
2.00
6700
026.
7716
3270
1.46
536.
28R
T90-
RH
B70
–48.
1161
.23
371.
4300
111.
9700
54.1
600
675.
0067
0002
7.73
1632
703.
2253
8.51
RT9
0-R
HB
70–4
8.11
61.3
537
3.07
0011
3.12
0054
.460
067
8.00
6700
028.
6916
3270
4.98
540.
74R
T90-
RH
B70
–48.
1061
.48
374.
7100
114.
2800
54.7
700
681.
0067
0002
9.65
1632
706.
7454
2.98
RT9
0-R
HB
70–4
8.07
61.6
137
6.34
0011
5.44
0055
.070
068
4.00
6700
030.
6016
3270
8.50
545.
21R
T90-
RH
B70
–48.
0561
.71
377.
9700
116.
6100
55.3
700
687.
0067
0003
1.55
1632
710.
2754
7.44
RT9
0-R
HB
70–4
8.04
61.8
137
9.60
0011
7.77
0055
.680
069
0.00
6700
032.
5016
3271
2.04
549.
67R
T90-
RH
B70
–48.
0361
.93
381.
2300
118.
9500
55.9
800
693.
0067
0003
3.45
1632
713.
8155
1.90
RT9
0-R
HB
70–4
8.00
62.0
438
2.85
0012
0.12
0056
.270
069
6.00
6700
034.
3916
3271
5.58
554.
13R
T90-
RH
B70
–47.
9862
.15
384.
4800
121.
3000
56.5
700
699.
0067
0003
5.33
1632
717.
3555
6.36
RT9
0-R
HB
70–4
7.96
62.2
738
6.10
0012
2.48
0056
.870
070
2.00
6700
036.
2616
3271
9.13
558.
59R
T90-
RH
B70
–47.
9762
.36
387.
7200
123.
6700
57.1
600
705.
0067
0003
7.19
1632
720.
9156
0.82
RT9
0-R
HB
70–4
7.98
62.4
438
9.34
0012
4.86
0057
.460
070
8.00
6700
038.
1216
3272
2.69
563.
04R
T90-
RH
B70
–47.
9862
.55
390.
9600
126.
0500
57.7
500
711.
0067
0003
9.05
1632
724.
4756
5.27
RT9
0-R
HB
70–4
7.96
62.6
939
2.57
0012
7.24
0058
.040
071
4.00
6700
039.
9716
3272
6.26
567.
50R
T90-
RH
B70
–47.
9162
.81
394.
1800
128.
4400
58.3
300
717.
0067
0004
0.89
1632
728.
0556
9.73
RT9
0-R
HB
70–4
7.84
62.9
639
5.80
0012
9.65
0058
.610
072
0.00
6700
041.
8016
3272
9.84
571.
95R
T90-
RH
B70
–47.
7963
.09
397.
4100
130.
8500
58.9
000
723.
0067
0004
2.71
1632
731.
6457
4.17
RT9
0-R
HB
70–4
7.76
63.2
239
9.02
0013
2.07
0059
.190
072
6.00
6700
043.
6216
3273
3.44
576.
39R
T90-
RH
B70
–47.
7263
.35
400.
6200
133.
2900
59.4
800
729.
0067
0004
4.53
1632
735.
2457
8.61
RT9
0-R
HB
70–4
7.69
63.4
640
2.23
0013
4.51
0059
.760
073
2.00
6700
045.
4316
3273
7.05
580.
83R
T90-
RH
B70
–47.
6863
.57
403.
8300
135.
7400
60.0
500
��
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
735.
0067
0004
6.33
1632
738.
8658
3.05
RT9
0-R
HB
70–4
7.67
63.6
740
5.44
0013
6.96
0060
.330
073
8.00
6700
047.
2316
3274
0.67
585.
27R
T90-
RH
B70
–47.
6563
.76
407.
0400
138.
2000
60.6
200
741.
0067
0004
8.12
1632
742.
4858
7.49
RT9
0-R
HB
70–4
7.63
63.8
440
8.63
0013
9.43
0060
.900
074
4.00
6700
049.
0116
3274
4.30
589.
70R
T90-
RH
B70
–47.
6263
.95
410.
2300
140.
6700
61.1
800
747.
0067
0004
9.90
1632
746.
1159
1.92
RT9
0-R
HB
70–4
7.60
64.0
441
1.83
0014
1.91
0061
.460
075
0.00
6700
050.
7816
3274
7.93
594.
13R
T90-
RH
B70
–47.
5864
.11
413.
4200
143.
1600
61.7
400
753.
0067
0005
1.67
1632
749.
7559
6.35
RT9
0-R
HB
70–4
7.61
64.1
741
5.02
0014
4.41
0062
.020
075
6.00
6700
052.
5516
3275
1.57
598.
56R
T90-
RH
B70
–47.
6964
.16
416.
6100
145.
6500
62.2
900
759.
0067
0005
3.43
1632
753.
3960
0.78
RT9
0-R
HB
70–4
7.77
64.0
541
8.20
0014
6.90
0062
.570
076
2.00
6700
054.
3116
3275
5.20
603.
00R
T90-
RH
B70
–47.
8163
.91
419.
7900
148.
1400
62.8
400
765.
0067
0005
5.20
1632
757.
0160
5.23
RT9
0-R
HB
70–4
7.80
63.8
342
1.38
0014
9.38
0063
.110
076
8.00
6700
056.
0916
3275
8.82
607.
45R
T90-
RH
B70
–47.
8563
.73
422.
9700
150.
6100
63.3
800
771.
0067
0005
6.98
1632
760.
6360
9.67
RT9
0-R
HB
70–4
7.89
63.6
742
4.56
0015
1.84
0063
.660
077
4.00
6700
057.
8716
3276
2.43
611.
90R
T90-
RH
B70
–47.
9263
.65
426.
1600
153.
0700
63.9
300
777.
0067
0005
8.76
1632
764.
2361
4.12
RT9
0-R
HB
70–4
7.93
63.6
142
7.75
0015
4.30
0064
.200
078
0.00
6700
059.
6616
3276
6.03
616.
35R
T90-
RH
B70
–47.
9863
.57
429.
3500
155.
5200
64.4
800
783.
0067
0006
0.55
1632
767.
8361
8.58
RT9
0-R
HB
70–4
8.03
63.5
743
0.94
0015
6.74
0064
.750
078
6.00
6700
061.
4416
3276
9.63
620.
81R
T90-
RH
B70
–48.
0663
.58
432.
5300
157.
9600
65.0
200
789.
0067
0006
2.33
1632
771.
4262
3.04
RT9
0-R
HB
70–4
8.09
63.5
743
4.12
0015
9.19
0065
.280
079
2.00
6700
063.
2316
3277
3.22
625.
27R
T90-
RH
B70
–48.
1263
.61
435.
7100
160.
4100
65.5
500
795.
0067
0006
4.12
1632
775.
0162
7.51
RT9
0-R
HB
70–4
8.11
63.6
643
7.30
0016
1.63
0065
.810
079
8.00
6700
065.
0116
3277
6.81
629.
74R
T90-
RH
B70
–48.
0863
.76
438.
8900
162.
8500
66.0
800
801.
0067
0006
5.89
1632
778.
6063
1.97
RT9
0-R
HB
70–4
8.02
63.8
844
0.47
0016
4.07
0066
.340
080
4.00
6700
066.
7816
3278
0.41
634.
20R
T90-
RH
B70
–47.
9563
.96
442.
0600
165.
3000
66.6
000
807.
0067
0006
7.66
1632
782.
2163
6.43
RT9
0-R
HB
70–4
7.87
64.0
244
3.64
0016
6.54
0066
.870
081
0.00
6700
068.
5416
3278
4.02
638.
66R
T90-
RH
B70
–47.
7864
.10
445.
2300
167.
7800
67.1
400
813.
0067
0006
9.42
1632
785.
8364
0.88
RT9
0-R
HB
70–4
7.69
64.1
744
6.82
0016
9.02
0067
.410
081
6.00
6700
070.
3016
3278
7.65
643.
10R
T90-
RH
B70
–47.
6264
.26
448.
4100
170.
2600
67.6
800
��
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
819.
0067
0007
1.18
1632
789.
4764
5.31
RT9
0-R
HB
70–4
7.57
64.4
044
9.99
0017
1.51
0067
.950
082
2.00
6700
072.
0516
3279
1.30
647.
53R
T90-
RH
B70
–47.
5264
.56
451.
5800
172.
7700
68.2
300
825.
0067
0007
2.92
1632
793.
1364
9.74
RT9
0-R
HB
70–4
7.48
64.6
945
3.17
0017
4.03
0068
.500
082
8.00
6700
073.
7916
3279
4.96
651.
95R
T90-
RH
B70
–47.
4564
.83
454.
7500
175.
3000
68.7
700
831.
0067
0007
4.65
1632
796.
8065
4.16
RT9
0-R
HB
70–4
7.43
64.9
745
6.33
0017
6.57
0069
.040
083
4.00
6700
075.
5116
3279
8.64
656.
37R
T90-
RH
B70
–47.
4165
.11
457.
9100
177.
8400
69.3
100
837.
0067
0007
6.37
1632
800.
4865
8.58
RT9
0-R
HB
70–4
7.38
65.2
745
9.49
0017
9.12
0069
.580
084
0.00
6700
077.
2216
3280
2.32
660.
79R
T90-
RH
B70
–47.
3465
.44
461.
0600
180.
4100
69.8
400
843.
0067
0007
8.06
1632
804.
1766
2.99
RT9
0-R
HB
70–4
7.30
65.5
346
2.64
0018
1.69
0070
.110
084
6.00
6700
078.
9016
3280
6.02
665.
20R
T90-
RH
B70
–47.
2365
.59
464.
2100
182.
9900
70.3
700
849.
0067
0007
9.74
1632
807.
8866
7.40
RT9
0-R
HB
70–4
7.14
65.6
546
5.78
0018
4.28
0070
.630
085
2.00
6700
080.
5916
3280
9.74
669.
60R
T90-
RH
B70
–47.
0765
.75
467.
3500
185.
5900
70.9
000
855.
0067
0008
1.42
1632
811.
6067
1.80
RT9
0-R
HB
70–4
7.02
65.8
546
8.92
0018
6.89
0071
.170
085
8.00
6700
082.
2616
3281
3.47
673.
99R
T90-
RH
B70
–46.
9665
.94
470.
4900
188.
2000
71.4
400
861.
0067
0008
3.10
1632
815.
3467
6.18
RT9
0-R
HB
70–4
6.93
66.0
447
2.06
0018
9.51
0071
.710
086
4.00
6700
083.
9316
3281
7.21
678.
37R
T90-
RH
B70
–46.
9066
.16
473.
6300
190.
8300
71.9
800
867.
0067
0008
4.76
1632
819.
0868
0.56
RT9
0-R
HB
70–4
6.84
66.3
047
5.20
0019
2.15
0072
.250
087
0.00
6700
085.
5816
3282
0.96
682.
75R
T90-
RH
B70
–46.
7766
.43
476.
7700
193.
4700
72.5
200
873.
0067
0008
6.40
1632
822.
8568
4.94
RT9
0-R
HB
70–4
6.72
66.5
247
8.34
0019
4.80
0072
.780
087
6.00
6700
087.
2216
3282
4.73
687.
12R
T90-
RH
B70
–46.
6866
.63
479.
9000
196.
1400
73.0
500
879.
0067
0008
8.04
1632
826.
6268
9.31
RT9
0-R
HB
70–4
6.66
66.7
648
1.46
0019
7.48
0073
.320
088
2.00
6700
088.
8516
3282
8.51
691.
49R
T90-
RH
B70
–46.
6366
.92
483.
0200
198.
8200
73.5
900
885.
0067
0008
9.66
1632
830.
4169
3.67
RT9
0-R
HB
70–4
6.59
67.0
948
4.58
0020
0.17
0073
.850
088
8.00
6700
090.
4616
3283
2.31
695.
85R
T90-
RH
B70
–46.
5467
.25
486.
1400
201.
5200
74.1
200
891.
0067
0009
1.26
1632
834.
2169
8.02
RT9
0-R
HB
70–4
6.47
67.4
148
7.69
0020
2.88
0074
.380
089
4.00
6700
092.
0516
3283
6.12
700.
20R
T90-
RH
B70
–46.
4367
.59
489.
2400
204.
2400
74.6
400
897.
0067
0009
2.84
1632
838.
0370
2.37
RT9
0-R
HB
70–4
6.40
67.7
749
0.79
0020
5.62
0074
.900
090
0.00
6700
093.
6216
3283
9.95
704.
55R
T90-
RH
B70
–46.
3467
.91
492.
3300
206.
9900
75.1
600
�8
Leng
th
(m)
Nor
thin
g(m
)Ea
stin
g(m
)El
evat
ion
(m)
Coo
rdS
yste
mIn
clin
atio
n(d
egre
es)
Bea
ring
(deg
rees
)Lo
calA
(m
)Lo
calB
(m
)Lo
calC
(m
)Ex
trap
olfl
ag
903.
0067
0009
4.40
1632
841.
8670
6.72
RT9
0-R
HB
70–4
6.28
68.0
349
3.88
0020
8.37
0075
.410
090
6.00
6700
095.
1816
3284
3.79
708.
88R
T90-
RH
B70
–46.
2668
.19
495.
4200
209.
7600
75.6
700
909.
0067
0009
5.95
1632
845.
7171
1.05
RT9
0-R
HB
70–4
6.23
68.3
449
6.96
0021
1.15
0075
.920
091
2.00
6700
096.
7216
3284
7.64
713.
22R
T90-
RH
B70
–46.
2068
.48
498.
4900
212.
5500
76.1
700
915.
0067
0009
7.48
1632
849.
5771
5.38
RT9
0-R
HB
70–4
6.13
68.6
250
0.03
0021
3.95
0076
.430
091
8.00
6700
098.
2316
3285
1.51
717.
55R
T90-
RH
B70
–46.
0568
.74
501.
5600
215.
3500
76.6
800
921.
0067
0009
8.99
1632
853.
4571
9.71
RT9
0-R
HB
70–4
5.98
68.8
350
3.09
0021
6.77
0076
.930
092
4.00
6700
099.
7416
3285
5.39
721.
86R
T90-
RH
B70
–45.
9568
.94
504.
6200
218.
1800
77.1
800
927.
0067
0010
0.49
1632
857.
3472
4.02
RT9
0-R
HB
70–4
5.88
69.0
950
6.15
0021
9.60
0077
.430
093
0.00
6700
101.
2416
3285
9.29
726.
17R
T90-
RH
B70
–45.
8269
.23
507.
6700
221.
0300
77.6
800
933.
0067
0010
1.98
1632
861.
2572
8.33
RT9
0-R
HB
70–4
5.77
69.3
850
9.20
0022
2.46
0077
.930
093
6.00
6700
102.
7216
3286
3.20
730.
47R
T90-
RH
B70
–45.
7369
.53
510.
7200
223.
8900
78.1
800
939.
0067
0010
3.45
1632
865.
1773
2.62
RT9
0-R
HB
70–4
5.68
69.6
951
2.24
0022
5.33
0078
.430
094
2.00
6700
104.
1816
3286
7.13
734.
77R
T90-
RH
B70
–45.
6269
.85
513.
7600
226.
7800
78.6
700
945.
0067
0010
4.90
1632
869.
1073
6.91
RT9
0-R
HB
70–4
5.55
70.0
251
5.27
0022
8.23
0078
.920
094
8.00
6700
105.
6216
3287
1.08
739.
05R
T90-
RH
B70
–45.
4970
.21
516.
7900
229.
6900
79.1
600
951.
0067
0010
6.33
1632
873.
0674
1.19
RT9
0-R
HB
70–4
5.42
70.3
651
8.30
0023
1.15
0079
.410
095
4.00
6700
107.
0416
3287
5.04
743.
33R
T90-
RH
B70
–45.
3570
.49
519.
8000
232.
6200
79.6
500
957.
0067
0010
7.74
1632
877.
0374
5.46
RT9
0-R
HB
70–4
5.26
70.6
452
1.31
0023
4.10
0079
.890
096
0.00
6700
108.
4416
3287
9.02
747.
60R
T90-
RH
B70
–45.
1570
.79
522.
8100
235.
5800
80.1
300
963.
0067
0010
9.14
1632
881.
0274
9.72
RT9
0-R
HB
70–4
5.05
70.9
552
4.32
0023
7.07
0080
.380
096
6.00
6700
109.
8316
3288
3.02
751.
85R
T90-
RH
B70
–44.
9671
.09
525.
8200
238.
5700
80.6
200
969.
0067
0011
0.52
1632
885.
0375
3.97
RT9
0-R
HB
70–4
4.88
71.2
552
7.32
0024
0.07
0080
.870
097
2.00
6700
111.
2016
3288
7.04
756.
08R
T90-
RH
B70
–44.
8071
.42
528.
8200
241.
5800
81.1
100
978.
0067
0011
2.55
1632
891.
0976
0.30
RT9
0-R
HB
70–4
4.68
71.6
753
1.80
0024
4.62
0081
.600
0
Prin
tout
from
SIC
AD
A 2
005-
10-2
0 14
:33:
16.
��
Appendix4
LengthreferencemarksReferenceMarkT–Referencemarkindrillhole
KFM06C,2005‑06‑2719:00:00–2005‑06‑2806:00:00(150.000–960.000m).
Bhlen(m)
Rotationspeed(rpm)
Startflow(l/min)
Stopflow(l/min)
Stoppressure(bar)
Cuttertime(s)
Tracedetectable
Cutterdiameter(mm)
Comment
150.00 400.00 250 350 28.0 1 Ja200.00 400.00 250 350 30.0 1 Ja
250.00 400.00 250 350 30.0 0 Ja300.00 400.00 250 350 30.0 0 Ja350.00 400.00 250 400 30.0 0 Ja400.00 400.00 300 400 30.0 1 Ja447.00 400.00 400 500 30.0 1 Ja500.00 400.00 400 550 35.0 0 Ja550.00 400.00 400 550 35.0 0 Ja600.00 400.00 400 550 35.0 0 Ja652.00 400.00 400 600 35.0 1 Ja700.00 400.00 400 600 40.0 0 Ja750.00 400.00 400 600 40.0 0 Ja800.00 400.00 450 600 40.0 1 Ja850.00 400.00 400 600 40.0 1 Ja898.00 400.00 400 600 40.0 0 Ja960.00 400.00 400 600 40.0 0 Ja
Printout from SICADA 2005-10-12 16:52:42.