mirage

Constraints on the origin and volume of gas in the New Albany Shale (Devonian – Mississippian), eastern Illinois Basin

DSpace/Manakin Repository

Show simple item record

dc.contributor.author Mastalerz, M
dc.contributor.author Drobniak, A
dc.contributor.author Rupp, JA
dc.contributor.author Strąpoć, D
dc.contributor.author Schimmelmann, A
dc.contributor.author Hasenmueller, NR
dc.date.accessioned 2010-10-15T17:25:29Z
dc.date.available 2010-10-15T17:25:29Z
dc.date.issued 2010-09-25
dc.identifier.uri http://hdl.handle.net/2022/9487
dc.description This poster was presented at the Eastern Section American Association of Petroleum Geologists (AAPG) conference in Kalamazoo, Michigan, September 25-29, 2010. en
dc.description.abstract This study investigates kerogen petrography, gas desorption, geochemistry, and micro- and mesoporosity of the New Albany Shale (Devonian-Mississippian) in the eastern part of the Illinois basin. Core analysis from two locations, one in Owen County, Indiana and one in Pike County, Indiana was conducted. The volumes of gas in the locations studied are primarily dependent on total organic carbon (TOC) content and the micropore volume of the shales. Gas origins were assessed using stable isotope geochemistry, whereas maturity assessments utilized both measured and modeled Ro values. Different depths of burial and formation water salinities are likely responsible for dominant origins of the gas in the two locations studied. The shallower Owen County location (415 to 433 m deep) contains significant microbial methane, whereas the Pike County location (832 to 860 m deep) is characterized exclusively by thermogenic gas. Despite differences in the gas origins, the total gas in both locations is similar, reaching up to 2.2 cm3/g (70 scf/ton). The lower thermogenic gas content at the shallower location (probably because of the lower thermal maturity and possibly higher loss of gas related to uplift and leakage via relaxed fractures) is compensated by additional generation of microbial methane most probably stimulated by influx of glacial meltwater causing both brine dilution and microbial inoculation. The characteristics of the shale of the Maquoketa Group (Ordovician) in the Pike County location indicate that the controls on the gas volumes are similar to those in the New Albany Shale. en
dc.language.iso en_US en
dc.rights This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/2.5/ or send a letter to Creative Commons, 543 Howard Street, 5th Floor, San Francisco, California, 94105, USA. en
dc.rights.uri http://creativecommons.org/licenses/by-nc-sa/2.5/ en
dc.subject isotopes en
dc.subject porosity en
dc.subject geochemistry en
dc.subject gas origin en
dc.subject shale gas en
dc.subject Illinois Basin en
dc.subject Indiana Geological Survey en
dc.subject New Albany Shale en
dc.title Constraints on the origin and volume of gas in the New Albany Shale (Devonian – Mississippian), eastern Illinois Basin en
dc.type Presentation en


Files in this item

This item appears in the following Collection(s)

Show simple item record

This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/2.5/ or send a letter to Creative Commons, 543 Howard Street, 5th Floor, San Francisco, California, 94105, USA. This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/2.5/ or send a letter to Creative Commons, 543 Howard Street, 5th Floor, San Francisco, California, 94105, USA.

Search IUScholarWorks


Advanced Search

Browse

My Account

Statistics