尼日尔三角洲坡脚逆冲带沉积样式及构造控制

李磊; 王英民; 张莲美; 黄志超

Volume 33 Issue 5

Sep. 2008

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Article Navigation > Earth Science > 2008 > 33(5): 643-650

LI Lei, WANG Ying-min, ZHANG Lian-mei, HUANG Zhi-chao, 2008. Sedimentary Patterns and Structural Control across Toe Thrust Belts, Niger Delta. Earth Science, 33(5): 643-650.

Citation:

LI Lei, WANG Ying-min, ZHANG Lian-mei, HUANG Zhi-chao, 2008. Sedimentary Patterns and Structural Control across Toe Thrust Belts, Niger Delta. Earth Science, 33(5): 643-650.

LI Lei, WANG Ying-min, ZHANG Lian-mei, HUANG Zhi-chao, 2008. Sedimentary Patterns and Structural Control across Toe Thrust Belts, Niger Delta. Earth Science, 33(5): 643-650.

Citation:

LI Lei, WANG Ying-min, ZHANG Lian-mei, HUANG Zhi-chao, 2008. Sedimentary Patterns and Structural Control across Toe Thrust Belts, Niger Delta. Earth Science, 33(5): 643-650.

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Sedimentary Patterns and Structural Control across Toe Thrust Belts, Niger Delta

1.
Faculty of Natural Resources & Information Technology, China University of Petroleum, Beijing 102249, China
2.
State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China
3.
School of Resources & Geosciences, China University of Mining & Technology, Xuzhou 221008, China
4.
Institute of SINOPEC Shanghai Offshore Oil & Gas Company, Shanghai 200092, China

Received Date: 2008-03-28
Publish Date: 2008-09-25

Abstract

Abstract

Researches on sedimentary patterns and structural control across toe thrust belts can demonstrate the distribution and evolution of deep-water sediments. In this paper, mechanism of limb rotation in growth strata and technique of seismic facies analysis are used. There are three features in the minibasins induced by gravitational sliding on the slope: the firstly, feature is surface of unconformity developed by onlap on minibasin margins or surface of unconformity truncated by mass-transport-complex are sequence boundary in the study area; the secondly, accommodation of gravity flow is controlled by uplift rate and sedimentation rate, and styles of filling in the minibasins are dominated by the interrelationship between the two factors; and the third, there are two stacking patterns that consists of upward of turbidite fan-hemipelagic drape mud or mass-transport complexes-turbidite fan-hemipelagic drape mud. Models showing evolution of sediment in Single minibasin and in multiple minibasins are built based on the study of uplift and rate of deposition.
- Niger Delta,
- toe thrust belts,
- growth strata,
- structural control,
- seismic facies

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References(34)

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