TRENTON/POINT PLEASANT/UTICA WOOD … C S Vf F E (9 9652 9650 9648 9646 9644 9642 9640 9638 9636 9634 9632 9630 9628 9626 9624 9622 9620 9618 9616 9614 9612 ... 2” thick brach hash

M C S Vf F

9652

9650

9648

9646

9644

9642

9640

9638

9636

9634

9632

9630

9628

9626

9624

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9534

9532

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9528

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9516

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9510

9508

9506

9504

9502

9500

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9492

9490

9488

9486

9484

9482

9480

9478

9476

9474

9472

9470

9468

9466

9464

9462

9460

9458

9456

9454

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9450

9448

9446

9444

9442

9440

9438

9436

9434

9432

9430

9428

9426

9424

9422

9420

9418

Sharply interlaminated skeletal packstone w/ non calcareous shale. Undulating scoured base, escape burrows, reworked rounded intraclasts

Sharp based skeletal packstone grading into grey micrite, rounded grey shale intraclasts

Steeply bedded biospar with thin shale partings ~ 0.5 cm

2” lag bed of highly reworked skeletal frag’s

Micrite, lenticular to HCS at top with thin shale partings, reworked fossil frag’s and skeletal grains

Sharp based skeletal packstone grading up into micrite

Bioclastic packstone hash beds sharply interlaminated w/ grey lime mudstone, more fossiliferous than below, more greater mudstone contentPackstones show graded bedding, scoured base

Sharp based skeletal packstone grading up unto crystalline sparite/micrite, greater lime mudstone content than below

Grey micrite gradationally interbedded with grey lime mudstone

Skeletal lag in micrite matrix, steeply/sharply bedded

Biomicrite w/ prasopora, brachs, shale partings ~ 1cm thick, wavy bedded

Biomicrite sharply interlaminated w/ grey-black lime mudstone, gradint up into grey lime mudstone w/ thin brach. layers

2” thick brach hash layer

Sharp based biomicrite to biosparite grading up into black marl, some marl intraclasts, brachs, crinoids

Bryozoans

Brachiopods

Intraclasts

Burrows

Wavy Lams

Cross Bedding

Crinoids

Soft sed def

Skel packstone w/ lt grey marl matrix, showing steep bedding and soft sed deformation in blk marl

3-5” biospar beds interlaminated with black marl, biospar drapes into marl, biospar show traction current bedding, some tiny brachs within marl

Grey marl, few brachs

Wavy bedded marl/micrite, sharp to gradational contacts with thin, wavy bioclast layers at base of micrite interbeds

Convolute interbedded dark grey marl and micrite, micrite interbeds thinner and darker than below, with greater percentage of marl

slightly fossiliferous

micrite interbeds pillow into marls

Micrite interbeds decreasing upward

Convolute bedded dark marl, skeletal packstone, and micrite marl drapes into micrite

Marl/micrite sharply, convolutely interbedded

Marl, churned w/ fossils, reworked dark micrite nodules 1” in diameter

Marl/dark micrite interbedded, wavy bedded, more gradational interbeds than below

Dark grey-black biomicrite, highly fossiliferous, wavy bedded, with few thin clean grey nodular micrite interbeds

PPL black marl

Thin nodular micrite, black marl drapes down into micrite bed

Massive bedded grey micrite, unfossiliferousPPL black marl

Black marl w/ micrite sharply interbedded, some 0.5” thick fossil hash horizons at top of marls, micrite shows low angle cross bedding

Black marl grading into massive bedded dark micrite

Black marl w/ thin 0.5” thick skeletal sand lenses that pinch and swell

Black marl, some thin lenses of carbonate sand/skeletal grains

frequent slickensides

Micrite interbed, dark grey, gradational top and base

Thin dark micrite interbed, PPL at base, gradational top

Calcareous black shale

Black shale, slightly calcareous, occasional thin skeletal lag interbed

Black mudstone, slightly calcareous

Black shale

Black shale, more calcareous than below

Black shale

Black shale, slightly calcareous, occasional thin skeletal beds containing crinoid pieces

Micrite interbed, sharp base, cross bedded at base grading up into PPL into black shale

Nodular micrite interbed

Black shale interbedded with light grey shale, becoming fossiliferous upward, crinoids

Grey shale, slightly calcareous, sparsely fossiliferous

Sed Struc Fossils

Key to Symbols

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LithostratSequence Strat

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MFS

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API #4710700351POWER OIL COMPANY #9634WOOD COUNTY, WVTRENTON/POINT PLEASANT/UTICACO

RE P

RESE

NTE

D IN

SH

OW

CASE

McClain, 2013, Sequence stratigraphy and petrophysics of the Late Ordovician Utica-Point Pleasant interval in the Central AppalachianBasin, eastern Ohio and western Pennsylvania.

9486

9492

9507.8

9525

9530.5

9543

9565.5

9571

9583

9599

Vitrinite Reflectance Measurements, Histogram and Images

Company: Core Lab - IRS Division/Hope Natural Gas Company List of Ro Values in Increasing Order:Formation: Utica 1.95 2.18 2.25Location: Wood Co., WVWell: Power Oil Company # 9634Depth (ft): 9448.00Min Value 1.95Max Value 2.25Mean Value 2.13# of Measurements 3 10 micrometersStrd Deviation 0.16

The mean Ro, ran of pyrobitumen is 2.13%based on 3 measurements. The VRo-equivalent is 1.72%. Organic matter is post-mature and in the dry gas window.

Plate 1 A-D

The above values were measured on pyrobitumen. The VRo-eq is estimated to be 1.72% using the Jacob formula (Rvit = Rbit x 0.618 + 0.4).

A

C D

B

Photo Captions:(A) Pyrobitumen (Pbit) (BRo,ran=2.219%).(B) Thin and elongated fragment of a zooclast (Zoo) encountered normal to bedding. (C) A broken fragment of a chitinozoan (Ch) showing the characteristic features, such as prosome (pr) and chamber (Cmb) (ChRo,ran=1.84%). (D) Thin-walled chitinozoan (Ch) showing the chamber (Cmb). P=Pyrite.

General Description: Organic matter (OM) is lean and occurs as pyrobitumen that occupies intergranular space; broken chitinozoan fragments having a pitted surface texture; minor amount of other zooclast fragments; and specks of bitumen staining. A mean Ro,ran of 2.13% measured on pyrobitumen gave an equivalent VRo of 1.72%. A mean Ro,ran of 1.84% measured on the pitted chitinozoan gave equivalent VRo values of 1.53% and 1.62%, using the correlations given by Tricker et al. (1992) (RoVit-eq=(RoChi – 0.08) / 1.152) and Bertrand and Malo (2001) (RoVit-eq=(RoChi – 0.014) / 1.127). All of these VRo values suggest that the organic matter is post-mature and in the dry gas stage of hydrocarbon generation and retention process. The matrix consists of quartz, carbonates, silt/clay, and pyrite.

0

0.4

0.8

1.2

1.6

2

1.3-1.5 1.5-1.7 1.7-1.9 1.9-2.1 2.1-2.3 2.3-2.5

Freq

uenc

y

Random Ro at 546 nm

Histogram

PbitCh

Cmb P

Pbit Zoo

Ch Ch

P

P P

pr

Cmb


Company: Core Lab - IRS Division/Hope Natural Gas Company List of Ro Values in Increasing Order:Formation: Utica 2.11Location: Wood Co., WVWell: Power Oil Company # 9634Depth (ft): 9481.30Min Value 2.11Max Value 2.11Mean Value 2.11# of Measurements 1 10 micrometersStrd Deviation N/A

An Ro, ran of 2.11% was measured onpyrobitumen. The VRo-equivalent is 1.70%.Organic matter is post-mature and in thedry gas window.

Plate 2 A-D

The above value was measured on pyrobitumen. The VRo-eq is estimated to be 1.70% using the Jacob formula (Rvit = Rbit x 0.618 + 0.4).

A

C D

B

Photo Captions:(A) Pyrobitumen (Pbit) in intergranular space (BRo,ran=2.111%). (B) Thin-walled chitinozoan (Ch) showing the chamber (Cmb). (C) Bitumen staining (Bit Stng) mixed with mineral matter. (D) Thin and elongated zooclast-like (Zoo) fragment. P=Pyrite.

General Description: Organic matter is lean and occurs as pyrobitumen; thin-walled broken chitinozoan fragments; minor amount of other zooclast fragments; and bitumen staining. A Ro,ran of 2.11% measured on pyrobitumen gave an equivalent VRo of 1.70%, which suggests that the organic matter is post-mature and in the dry gas window. The matrix consists of quartz, carbonates, silt/clay, and pyrite.

0

0.2

0.4

0.6

0.8

1

1.7-1.9 1.9-2.1 2.1-2.3 2.3-2.5

Freq

uenc

y

Random Ro at 546 nm

Histogram

Pbit

P

Pbit Ch

Bit Stng

Zoo

Cmb


Company: Core Lab - IRS Division/Hope Natural Gas Company List of Ro Values in Increasing Order:Formation: Utica 1.99 2.03 2.07 2.10 2.12 2.15Location: Wood Co., WVWell: Power Oil Company # 9634Depth (ft): 9541.40Min Value 1.99Max Value 2.15Mean Value 2.08# of Measurements 6 10 micrometersStrd Deviation 0.06

The mean Ro, ran of pyrobitumen is 2.08%based on 6 measurements. The VRo-equivalent is 1.69%. Organic matter is post-mature and in the dry gas window.

Plate 3 A-D

The above values were measured on pyrobitumen. The VRo-eq is estimated to be 1.69% using the Jacob formula (Rvit = Rbit x 0.618 + 0.4).

A

C D

B

Photo Captions:(A) Pyrobitumen (Pbit) surrounding mineral matter (BRo,ran=2.077%). (B) Thin and elongated zooclast (Zoo). (C) Bitumen staining (Bit Stng) mixed with carbonate mineral matter (C). (D) Granular bitumen (Grnl Bit) in intergranular space. P=Pyrite.

General Description: Organic matter is lean and comprises pyrobitumen, minor amount of zooclast fragments, granular bitumen, and bitumen staining. A Ro,ran of 2.08% measured on pyrobitumen gave an equivalent VRo of 1.69%, which suggests that the organic matter is post-mature and in the dry gas window. The matrix is calcareous and consists of quartz, silt/clay, and pyrite.

0

1

2

3

4

5

6

1.6-1.8 1.8-2 2-2.2 2.2-2.4

Freq

uenc

y

Random Ro at 546 nm

Histogram

Pbit

C

P

Pbit Zoo

Bit Grnl Bit

C

C

P

P

P


Company: Core Lab - IRS Division/Hope Natural Gas Company List of Ro Values in Increasing Order:Formation: Utica 1.90 1.91 1.91 1.97 2.00 2.04 2.13 2.13 2.14 2.18Location: Wood Co., WV 2.24 2.39Well: Power Oil Company # 9634Depth (ft): 9588.00Min Value 1.90Max Value 2.39Mean Value 2.08# of Measurements 12 10 micrometersStrd Deviation 0.15

The mean Ro, ran of chitinozoans is 2.08%based on 12 measurements. The VRo-equivalent is 1.74%. The organic matter ispost-mature and in the dry-gas window.

Plate 4 A-D

The above values were measured on chitinozoan fragments. The VRo-eq is estimated to be 1.74% using the correlation of Tricker et al. (1992) (RoVit-eq=(RoChi – 0.08) / 1.152).

A

C D

B

Photo Captions:(A) Pyrobitumen (Pbit) in intergranular space (BRo,ran=2.104%). P=Pyrite.(B) A broken part of a chitinozoan (Ch) showing the basal edge (be) (slightly out of focus because of its orientation) (ChRo,ran=2.023%). (C) Broken chitinozoan (Ch) (ChRo,ran=1.968%). (D) Chitinozoan (Ch) showing chamber (Cmb) (ChRo,ran=1.903%).

General Description: This sample is rich in broken parts of chitinozoans. Organic matter also occurs as trace pyrobitumen and bitumen staining. A mean Ro,ran of 2.08% measured on chitinozoans was used to obtain an equivalent VRo of 1.74% using the correlation given by Tricker et al. (1992). The same mean Ro,ran on chitinozoans gave an equivalent VRo of 1.83% using the correlation given by Bertrand and Malo (2001). Also, a Ro,ran of 2.11% measured on a single reliable grain of pyrobitumen gave an equivalent VRo of 1.70%. All of these equivalent VRo values suggest that the organic matter is post-mature and in the dry gas window. The matrix is calcareous and more argillaceous than the previous samples, and contains pyrite.

0

1

2

3

4

5

6

1.2-1.4 1.4-1.6 1.6-1.8 1.8-2 2-2.2 2.2-2.4 2.4-2.6

Freq

uenc

y

Random Ro at 546 nm

Histogram

Ch

Pitted Ch

Pbit

P

be

Pbit Ch

Ch Ch

P

P

Cmb

Images and Captions Continued

Company: Core Lab - IRS Division/Hope Natural Gas CompanyFormation: UticaLocation: Wood Co., WVWell: Power Oil Company # 9634Depth (ft): 9588.00

10 micrometers

Plate 4 E-H

E

G H

F

Photo Captions:(E) Thin-walled chitinozoan (Ch) showing characteristic features, such as prosome (pr) and chamber (Cmb). (F) Thick-walled chitinozoan (Ch) showing the chamber (Cmb) and prosome (pr). Mean Ro,ran is 2.035%. (G) Same as in (E), but missing the chamber. (H) A zooclast (Zoo) fragment that was replaced by pyrite partially. A relic of the precursor is still visible. P=Pyrite.

P

Ch Ch

Ch Zoo

Cmb

Cmb

Pr

P

P P

Pr

Pr

Client: Core LaboratoriesField/Well: Job # 150705

Geomark ID: RCOR-151105Source Rock Analyses

3

GeoMark Source Rock Services218 Higgins StreetHumble, TX 77338

(832) 644.1184info@ geomarkresearch.com

November 13, 2015

Core Laboratories Hope Power Co. 9634,

Total Organic Carbon Oil Potential, S2 Hydrogen Index, S2/TOC

9,350

9,400

9,450

9,500

9,550

9,600

9,650

9,700

9,750

9,8000 5 10 15 20

Mea

sure

d D

epth

, MD

(ft)

Oil Potential S2 (mg HC/g)

Good - ExcellentPoor Fair9,350

9,400

9,450

9,500

9,550

9,600

9,650

9,700

9,750

9,8000 200 400 600 800 1000

Mea

sure

d D

epth

, MD

(ft)

Hydrogen Index, S2/TOC

Oil (Type II)Gas Mixed Oil (Type I)

SOURCE ROCK ANALYSESGEOMARK GEOMARK RESEARCH, LTD.

0 20 40 60 80 1009,350

9,400

9,450

9,500

9,550

9,600

9,650

9,700

9,750

9,8000 2 4 6 8 10 12

Mea

sure

d D

epth

, MD

(ft)

Total Organic Carbon (wt%)

TOC

% Carbonate

% Carbonate

GoodPoor Fair Excellent



4



November 13, 2015


Norm. Oil Content, S1/TOC Production Index, S1/(S1+S2) Maturity Indicators

9,350

9,400

9,450

9,500

9,550

9,600

9,650

9,700

9,750

9,8000.00 0.25 0.50 0.75 1.00

Mea

sure

d D

epth

, MD

(ft)

Production Index, S1/(S1+S2)

Gas Generation

Imm

atur

e

Oil Gen.

415 435 455 475 495 515 5359,350

9,400

9,450

9,500

9,550

9,600

9,650

9,700

9,750

9,8000.2 0.8 1.4 2.0 2.6 3.2

Mea

sure

d D

epth

, MD

(ft)

Vitrinite Reflectance (or VR Equivalent)

Measured %Ro

Calculated %Ro

Tmax

Gas Generation

Imm

atur

e

Oil Generation

Tmax (°C)


0 20 40 60 80 1009,350

9,400

9,450

9,500

9,550

9,600

9,650

9,700

9,750

9,8000 50 100 150 200 250 300

Mea

sure

d D

epth

, MD

(ft)

Normalized Oil Content, S1/TOC

S1/TOC

% Carbonate

% Carbonate

Low

Mat

urity

Ear

ly M

atur

e

Mature / Stained

Oil / Gas Production or Contamination



5



November 13, 2015


Pseudo Van Krevelen Plot


0

100

200

300

400

500

600

700

800

900

1000

0 20 40 60 80 100 120 140 160 180 200

Hyd

roge

n In

dex

(mg

HC

/ g

TOC

)

Oxygen Index (mg CO2 / g TOC)

TYPE I KEROGEN

TYPE II KEROGEN

TYPE III KEROGEN

TYPE IV KEROGEN



6



November 13, 2015


Kerogen Quality Plot

0

10

20

30

40

50

60

0 2 4 6 8 10 12 14 16

Rem

aini

ng H

ydro

carb

on P

oten

tial,

S2 (m

g H

C /

g R

ock)

Total Organic Carbon, TOC (wt %)

Type I: Oil ProneUsually Lacustrine

Type III: Gas Prone

Mixed Type II / III:Oil / Gas Prone

Type II: Oil ProneUsually Marine

Dry Gas Prone

HI = 50

HI = 200

HI = 350

HI = 700




7



November 13, 2015


Kerogen Type and Maturity

0

200

400

600

800

1000

400 410 420 430 440 450 460 470 480 490 500

Hyd

roge

n In

dex

(mg

HC

/ g

TOC

)

Tmax (°C)

TYPE I KEROGEN

TYPE II KEROGEN

TYPE III KEROGEN


~ 0.6 % Ro ~ 1.4 % Ro

Immature Oil Generation Gas Generation



8



November 13, 2015


Kerogen Quality Plot


0.00

0.10

0.20

0.30

0.40

0.50

0.60

0.70

0.80

0.90

1.00

380 400 420 440 460 480 500 520 540 560 580 600

Ker

ogen

Con

vers

ion,

PI (

S1/(S

1+S2

)

Tmax (C)

Immature Dry Gas ZoneOil Zone CondensateWet Gas

Zone

Stained or Contaminated

Low Level Conversion

0

0.5

1

1.5

2

2.5

3

3.5

4

4.5

280330380430480530

Dep

th (k

m)

Age (Ma)

Depth subsidence curves and backstripped tectonic subsidence for the Appalachian Basin

Appalachian Basin -Tectonic SubsidenceTotal SubsidenceCompacted Sediment Curve

9427

Nodular packstone; nodules separated by pressure solution. Some nodules contain large fossil fragments, while others are clay-rich and largely devoid of fossils

Fossiliferous black shale with burrows; fossils are in lenses that do not follow bedding planes

Fossiliferous black shale with thin event bed (turbidite/storm?). Small, densely packed fossils

Interbedded grainstone and packstone with slight internal grading and grain size changes between beds

Micrite with elongated organics. Burrowed/bioturbated. Fossils unique when comparedto surrounding strata. Contains a geopetal ostracod (?) with pyrite and calcite

Echinoderm packstone with claystone lenses. Lenses contain pyrite framboids, Fe-oxides anddead oil. Echinoderms show pressure solution features between grains and mud

Micrite with pyrite framboids. Bioturbated--one small burrow observed �lled with pyrite(sometimes re-oxidized to iron oxide) and calcite. Sponge spicules observed.

Fossiliferous black shale with high organic content. Pyrite framboids observed; pyritereplaces some fossil material (e.g. trilobite in �rst image). Bioturbated with lenses of fossil fragments

Black shale with calcite intraclast. Finely laminated claystone and siltstone. Claystonesare partially burrowed with trilobite and ostracode fragments. Siltstone is burrowedand contains a calcite intraclast with burrows and well-formed pyrite. Black shale at base contains ~25% ostracodes, tightly packed

Black shale with peloids and faint burrows. Fossil walls are very thin. Fossils and peloids show extensive post-diagensis distortion and compaction

Black shale, �ssile and �nely laminated. Scattered echinoderm and trilobite fragments. Organic debris is elongated and oriented parallel to bedding.

NW Boundary Flt s

ys

Burn

ing

Sprin

gs

NW Boundary Flt

SE B

ndry

Flt

Tyler

Wetzel

Ritchie

Marshall

Harrison

Wood Doddridge

Ohio

Marion

Pleasants

Brooke

LewisWirt

Monongalia

POWER OIL CO #9634 LOCATION MAP

Power_Oil_Co_9634_Location

Rome Trough Boundary Faults & Burning Springs Anticline

Permitted WV Utica

Completed WV Utica

WV Counties Core Laboratories - IRS DivisionPower Oil Company #9634

Composition Determined by XRD & TOC File: 150705G

Core LaboratoriesIntegrated Reservoir Solutions

Depth 9421.20 9430.70 9448.00 9458.60 9462.00 9470.60 9481.30 9490.60 9502.00 9511.10 9521.60 9530.40 9541.40 9552.70Weight % TOC 0.37 0.35 0.38 0.42 0.29 0.36 0.37 0.85 2.18 2.36 1.34 0.31 0.18 0.33Weight % Mineralogy(without TOC)Whole Rock DataQuartz 20.1 18.2 19.1 18.8 14.9 16.0 17.9 16.4 23.7 18.2 16.3 5.3 4.4 18.1Plagioclase 5.9 5.3 5.9 6.9 6.9 4.4 4.8 5.2 8.1 6.3 5.4 1.8 1.7 6.7Calcite 15.8 29.3 22.6 23.2 31.0 30.9 26.8 34.3 21.3 33.8 34.5 81.5 82.2 18.6Dolomite & Fe- Dolomite 0.7 0.9 0.7 0.8 1.3 1.7 1.3 0.6 0.6 1.5 1.7 0.0 0.6 5.6Pyrite 1.8 2.2 1.7 2.0 2.1 2.8 3.2 3.5 2.8 3.2 2.0 1.4 1.2 2.3Total Clay 55.8 44.1 49.9 48.3 43.9 44.2 46.1 39.9 43.5 37.2 40.0 10.0 10.0 48.6Relative Clay DataIllite/Smectite* 5.8 5.7 5.4 8.0 7.2 6.6 7.3 8.8 6.1 9.4 8.5 13.5 13.7 6.6Illite & Mica 46.2 41.9 47.3 42.9 46.0 45.6 45.0 44.8 51.4 48.2 48.1 48.9 63.3 50.9Chlorite 48.0 52.4 47.3 49.1 46.8 47.8 47.7 46.4 42.5 42.3 43.4 37.6 23.0 42.4Sum Bulk 100.1 100.0 99.9 100.0 100.1 100.0 100.1 99.9 100.0 100.2 99.9 100.0 100.1 99.9Sum Clay 100.0 100.0 100.0 100.0 100.0 100.0 100.0 100.0 100.0 99.9 100.0 100.0 100.0 99.9Volume % Mineralogy(includes TOC as Kerogen)Quartz 20.6 18.8 19.6 19.4 15.3 16.6 18.5 16.8 23.3 17.9 16.4 5.4 4.5 18.7Plagioclase 6.1 5.6 6.1 7.1 7.2 4.6 5.0 5.3 8.0 6.2 5.5 1.9 1.7 7.0Calcite 15.9 29.5 22.7 23.3 31.2 31.3 27.1 34.3 20.6 32.5 33.9 81.4 82.2 18.8Dolomite & Fe- Dolomite 0.6 0.8 0.7 0.8 1.2 1.6 1.2 0.6 0.5 1.3 1.6 0.0 0.5 5.4Pyrite 1.0 1.2 0.9 1.1 1.1 1.5 1.7 1.9 1.5 1.6 1.1 0.8 0.6 1.2Illite/Smectite* 3.4 2.6 2.8 4.0 3.3 3.0 3.5 3.6 2.7 3.5 3.5 1.4 1.4 3.4Illite & Mica 26.3 18.9 24.1 21.1 20.6 20.7 21.3 18.1 21.9 17.5 19.1 4.9 6.4 25.3Chlorite 25.2 21.8 22.2 22.3 19.3 19.9 20.8 17.3 16.6 14.1 15.9 3.5 2.1 19.4Kerogen 0.9 0.8 0.9 1.0 0.7 0.8 0.9 2.0 4.9 5.3 3.1 0.7 0.4 0.8Total 100.0 100.0 100.0 100.1 99.9 100.0 100.0 99.9 100.0 99.9 100.1 100.0 99.8 100.0Vclay 54.9 43.3 49.1 47.4 43.2 43.6 45.6 39.0 41.2 35.1 38.5 9.8 9.9 48.1Calc. G.D. (g/cc) 2.738 2.743 2.733 2.735 2.739 2.749 2.752 2.735 2.674 2.675 2.699 2.716 2.716 2.743

* Mixed-Layer Illite/Smectite Contains 10-15% Smectite Layers

Subsidence curve constructed by University of Cincinnati Basin Dynamics class (2012) using data from the Power Oil Company under the supervision of Dr. Paul Potter and Dr. Carlton Brett

REGIONAL STRATIGRAPHIC NOMENCLATURE

CORELAB VRo REPORT LOCATION MAP

CORELAB XRD ANALYSES

CORELAB SOURCE ROCK ANALYSES

THIN SECTION DESCRIPTIONS

Documents

TRENTON/POINT PLEASANT/UTICA WOOD … C S Vf F E (9 9652 9650 9648 9646 9644 9642 9640 9638 9636 9634 9632 9630 9628 9626 9624 9622 9620 9618 9616 9614 9612 ... 2” thick brach hash