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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
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
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
http://www.marcellus.psu.edu/resources/PDFs/DCNR.pdf
Geologic Settings
http://eg.geoscienceworld.org/content/18/4/21
7/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.
Smith Core
Location:
41°12'36.02"N
77°12'18.35"W
Methods
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
• 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
• 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
Well Location MapMethods
Results
125
145
165
185
205
225
245
265
285
305
0.0 1.0 2.0 3.0 4.0 5.0
Depth(ft)
%TOC
Depth Vs %TOC
Results
Results
Results
Results
Thickness
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
Acknowledgements
• Dr. Rudy Slingerland
• The Undergraduate Research Fund
• Anna Wendt
• Courtney Swanson

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CEL Thesis Presentation

  • 1. 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
  • 2. 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
  • 3. 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
  • 5. http://eg.geoscienceworld.org/content/18/4/21 7/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.
  • 7. 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
  • 8. • 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
  • 9. • 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
  • 11. Results 125 145 165 185 205 225 245 265 285 305 0.0 1.0 2.0 3.0 4.0 5.0 Depth(ft) %TOC Depth Vs %TOC
  • 16. 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
  • 17. Acknowledgements • Dr. Rudy Slingerland • The Undergraduate Research Fund • Anna Wendt • Courtney Swanson