globalchange  > 过去全球变化的重建
DOI: 10.1306/07071413232
Scopus记录号: 2-s2.0-84922590643
论文题名:
Eaglebine play of the southwestern East Texas basin Stratigraphic and depositional framework of the Upper Cretaceous (Cenomanian-Turonian) Woodbine and Eagle Ford Groups
作者: Hentz T.F.; Ambrose W.A.; Smith D.C.
刊名: AAPG Bulletin
ISSN: 0149-1570
EISSN: 1558-9300
出版年: 2014
发表日期: 2014
卷: 98, 期:12
起始页码: 2551
结束页码: 2580
语种: 英语
Scopus关键词: Arches ; Deposition ; Radioactivity logging ; Sandstone ; Shale ; Stratigraphy ; Cenomanian-Turonian ; East texas ; Hydrocarbon production ; Thickening zone ; Upper Cretaceous ; Gamma rays ; biostratigraphy ; Cenomanian ; depositional environment ; hydrocarbon exploration ; hydrocarbon reservoir ; sandstone ; succession ; Turonian ; Chihuahua ; Mexico [North America] ; Oklahoma [United States] ; San Marcos [Chihuahua] ; United States ; Washita Basin ; Parthenocissus quinquefolia
Scopus学科分类: Energy ; Earth and Planetary Sciences
英文摘要: The Woodbine and Eagle Ford Groups of the southwestern East Texas basin compose an emerging play, which has generated considerable interest because of its potential for new hydrocarbon production from both sandstone and mudrock reservoirs. However, the play's stratigraphic and depositional relations are complex and directly relate to the play's exploration challenges. Productive Woodbine and Eagle Ford (sub-Clarksville) sandstones intertongue with a poorly defined, subregional mudrock-dominated interval that thins southwestward toward the San Marcos arch. We propose dividing this succession into two intervals: (1) the Lower unit, a high-gamma-ray unit at the base of this mudrock succession that is inferred to be equivalent to the Maness Shale of the Washita Group and to part of the lower Eagle Ford Group on the San Marcos arch, and (2) an Upper unit, a basinward-thickening zone of consistently lower gamma-ray-log facies inferred to be equivalent to the Woodbine Group, Pepper Shale, and the Eagle Ford Group of the East Texas basin. Because the Cenomanian-Turonian boundary occurs within the Eagle Ford Group of the East Texas basin and the lower Eagle Ford section of the San Marcos arch, most of the Maness-through-Eagle Ford succession exists as a much-thinned section on the arch. Copyright © 2014. The American Association of Petroleum Geologists. All rights reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84922590643&doi=10.1306%2f07071413232&partnerID=40&md5=918140230545be1c08b8a33f5f8204e8
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/13141
Appears in Collections:过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响

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Recommended Citation:
Hentz T.F.,Ambrose W.A.,Smith D.C.. Eaglebine play of the southwestern East Texas basin Stratigraphic and depositional framework of the Upper Cretaceous (Cenomanian-Turonian) Woodbine and Eagle Ford Groups[J]. AAPG Bulletin,2014-01-01,98(12)
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