globalchange  > 过去全球变化的重建
DOI: 10.130C/091411U035
Scopus记录号: 2-s2.0-84860733835
论文题名:
The lateral strike-slip domain in gravitational detachment delta systems: A case study of the northwestern margin of the niger delta
作者: Leduc A.M.; Davies R.J.; Densmore L.A.; Imber J.
刊名: AAPG Bulletin
ISSN: 0149-1781
EISSN: 1558-9511
出版年: 2012
发表日期: 2012
卷: 96, 期:4
起始页码: 709
结束页码: 728
语种: 英语
Scopus关键词: Deepwater ; Fault system ; Fold-and-thrust belts ; Gravitational collapse ; Horizontal displacements ; Lateral expansion ; Niger Delta ; Possible futures ; Seismic datas ; Strike-slip fault systems ; Deformation ; Gravitational effects ; Strike-slip faults ; Tectonics ; Structural geology ; deep water ; deformation mechanism ; detachment fault ; estimation method ; gravity field ; strike-slip fault ; three-dimensional modeling ; thrust fault ; two-dimensional modeling ; Niger Delta ; Nigeria
Scopus学科分类: Energy ; Earth and Planetary Sciences
英文摘要: We use two- and three-dimensional seismic data to describe the structural geology of the lateral margin of a deep-water delta lobe within the Niger Delta that has undergone basinward, gravitationally driven translation. We term this region the "lateral strike-slip domain." Deformation is characterized by a strike-slip fault system that can be followed for a distance of approximately 75 km (~47 mi) from the shelf to the slope and toe of slope. On the northwestern side of the fault system, a fold and thrust belt that propagated north to northwest has developed within a large-scale restraining area of 460 km 2(180 mi 2). On the southeastern side of the strike-slip fault system, widespread extension has occurred, characterized by several graben and kilometer-scale rollover structures. Lateral margins of gravitational collapses give key information on how they deformed. We estimate a minimum horizontal displacement on the main strike-slip fault of approximately 7 km (~4 mi). Structural and kinematic evidence, such as presentday propagating strike-slip faults, for possible future lateral expansions of the lateral strike-slip domain, is described. We expect to observe similar sets of deformation styles at the margins of other preserved gravitational collapse sliding over a detachment whose efficiency in causing downdip slip may vary laterally. Copyright ©2012. The American Association of Petroleum Geologists. All rights reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84860733835&doi=10.130C%2f091411U035&partnerID=40&md5=3dd2a71bf522767f08a33e367256188b
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/13351
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:
Leduc A.M.,Davies R.J.,Densmore L.A.,et al. The lateral strike-slip domain in gravitational detachment delta systems: A case study of the northwestern margin of the niger delta[J]. AAPG Bulletin,2012-01-01,96(4)
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