cel thesis presentation

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Cory Lader Advisor: Dr. Rudy Slingerland Appalachian Basin Black Shale Group Department of Geosciences The Pennsylvania State University Distribution of Organic Carbon in the early Late Devonian Burket Member of the Harrell Formation in Pennsylvania

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Page 1: CEL Thesis Presentation

Cory LaderAdvisor: Dr. Rudy Slingerland

Appalachian Basin Black Shale GroupDepartment of Geosciences

The Pennsylvania State University

Distribution of Organic Carbon in the early Late Devonian

Burket Member of the Harrell Formation in Pennsylvania

Page 2: CEL Thesis Presentation

Introduction

- The Marcellus Currently Produces roughly 66.5 Bcf/d - Lower Union Spring Mbr.

- Several thousand feet above Marcellus lies another black shale- the Burket Mbr.- Potential to become the next

hot spot for oil and gas production

Page 3: CEL Thesis Presentation

Question– Is the Burket Mbr. in PA of sufficient organic richness and

thickness to warrant production?

Approach– Define the Total Organic Carbon (TOC) within the Burket Mbr. in

one core– Develop a function relating %TOC to total gamma ray count

measured in API units– Use the API values from 446 well logs, located throughout

Pennsylvania, to generate a map of the distribution of TOC and thickness of the potential pay zone

Research Objectives

Page 4: CEL Thesis Presentation

http://www.marcellus.psu.edu/resources/PDFs/DCNR.pdf

Geologic Settings

Page 5: CEL Thesis Presentation

http://eg.geoscienceworld.org/content/18/4/217/F5.large.jpg

Stratigraphic Relationships

- Early Late Devonian Black Shale- Underlain by the Tully Limestone- Black Shale Member of the Harrell

Fm.- Overlain by the Brallier Fm.- Thickest in NE Pa, thins to the SW- Interfingering with the Harrell Fm.

Page 6: CEL Thesis Presentation

Smith CoreLocation:

41°12'36.02"N 77°12'18.35"W

Methods

Page 7: CEL Thesis Presentation

Tully Limestome

Tully Limestone – Burket Member Contact

Burket Member

Burket Member – Brallier Formation Contact

Brallier Formation

The Smith Core and its inferred lithological features

Methods

Page 8: CEL Thesis Presentation

• Samples taken every foot starting at 125.1 ft and ending at 307.1 ft

• Sampling interval includes all of the Burket member and some of the Tully Limestone and Brallier Formation

• Interval includes a variety of TOC values to produce accurate results

Methods

Page 9: CEL Thesis Presentation

• All samples were powdered using a silica nitride vial in a Spex 8000 Ball Mill/Mixer and passed through stainless steel sieve

• Powdered samples were decarbonated by reacting the powdered samples with 10% Hydrochloric Acid (HCl) for 48 hours

• Following decarbonation, they were analyzed for TOC using an UIC, Inc. 5014 CO2 Coulometer with a 5200 Autosampler

Methods

Page 10: CEL Thesis Presentation

Well Location MapMethods

Page 11: CEL Thesis Presentation

Results

0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5 5.0125

145

165

185

205

225

245

265

285

305

Depth Vs %TOC%TOC

Dep

th (ft

)

Page 12: CEL Thesis Presentation

Results

Page 13: CEL Thesis Presentation

Results

Page 14: CEL Thesis Presentation

Results

Page 15: CEL Thesis Presentation

Results

Thickness

Page 16: CEL Thesis Presentation

Conclusions

• %TOC values of Burket Mbr. Hot spot are greater then 1% (1%= economic)

• Highest %TOC concentrations reside in Tioga, Potter, and Bradford County

• Potential production hot spots range in thickness from 45ft to 85ft• %TOC decreases in the Smith Core due to clastic dilution

Page 17: CEL Thesis Presentation

Acknowledgements

• Dr. Rudy Slingerland• The Undergraduate Research Fund• Anna Wendt• Courtney Swanson