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Reservoir Quality and Well Performance Analysis in the Middle Member of the Lewis Shale, Greater Green River Basin, Wyoming.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Reservoir Quality and Well Performance Analysis in the Middle Member of the Lewis Shale, Greater Green River Basin, Wyoming./
作者:
Mayorga-Gonzalez, Ligia Carolina.
面頁冊數:
1 online resource (278 pages)
附註:
Source: Dissertations Abstracts International, Volume: 84-05, Section: B.
Contained By:
Dissertations Abstracts International84-05B.
標題:
Geology. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=29068754click for full text (PQDT)
ISBN:
9798352693742
Reservoir Quality and Well Performance Analysis in the Middle Member of the Lewis Shale, Greater Green River Basin, Wyoming.
Mayorga-Gonzalez, Ligia Carolina.
Reservoir Quality and Well Performance Analysis in the Middle Member of the Lewis Shale, Greater Green River Basin, Wyoming.
- 1 online resource (278 pages)
Source: Dissertations Abstracts International, Volume: 84-05, Section: B.
Thesis (Ph.D.)--Colorado School of Mines, 2022.
Includes bibliographical references
The Lewis Shale is a turbidite system encompassing sandstones, siltstones, and organic-rich shales, deposited during the last Cretaceous seaway transgression. It is informally subdivided into three members; a lower member (characterized by high clay and organic matter content), a middle member or Dad sandstone member (a mixture of siltstones, shales, and sandstones), and an upper member (with decreasing amounts of sandstone and greenish grey shale s) that can reach up to 2600 ft in thickness. Its lithological characteristics vary depending upon its location within the Lewis Shale depositional basin (eastern Greater Green River Basin).The present study is in Sweetwater and Carbon counties in Wyoming . Data includes three cores in the Great Divide Basin and one on the Wamsutter Arch provided by MorningStar Partners/Southland Royalty. Cores contain various lithologies, including shales, siltstones, and sandstones, representing the Lewis Shale's lithologic heterogeneity and complexity.
Electronic reproduction.
Ann Arbor, Mich. :
ProQuest,
2023
Mode of access: World Wide Web
ISBN: 9798352693742Subjects--Topical Terms:
516570
Geology.
Subjects--Index Terms:
Environmental restrictionsIndex Terms--Genre/Form:
542853
Electronic books.
Reservoir Quality and Well Performance Analysis in the Middle Member of the Lewis Shale, Greater Green River Basin, Wyoming.
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The Lewis Shale is a turbidite system encompassing sandstones, siltstones, and organic-rich shales, deposited during the last Cretaceous seaway transgression. It is informally subdivided into three members; a lower member (characterized by high clay and organic matter content), a middle member or Dad sandstone member (a mixture of siltstones, shales, and sandstones), and an upper member (with decreasing amounts of sandstone and greenish grey shale s) that can reach up to 2600 ft in thickness. Its lithological characteristics vary depending upon its location within the Lewis Shale depositional basin (eastern Greater Green River Basin).The present study is in Sweetwater and Carbon counties in Wyoming . Data includes three cores in the Great Divide Basin and one on the Wamsutter Arch provided by MorningStar Partners/Southland Royalty. Cores contain various lithologies, including shales, siltstones, and sandstones, representing the Lewis Shale's lithologic heterogeneity and complexity.
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