二连盆地巴音都兰凹陷反转构造及成因机制

陈树光; 张以明; 崔永谦; 肖阳; 秦凤启; 吕德胜; 祖志勇; 李勇

doi:10.3799/dqkx.2017.044

Volume 42 Issue 4

Apr. 2017

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Article Navigation > Earth Science > 2017 > 42(4): 559-569

Chen Shuguang, Zhang Yiming, Cui Yongqian, Xiao Yang, Qin Fengqi, Lü Desheng, Zu Zhiyong, Li Yong, 2017. The Inversion Structures and Their Genetic Mechanisms of Bayindulan Sag, Erlian Basin. Earth Science, 42(4): 559-569. doi: 10.3799/dqkx.2017.044

Citation:

Chen Shuguang, Zhang Yiming, Cui Yongqian, Xiao Yang, Qin Fengqi, Lü Desheng, Zu Zhiyong, Li Yong, 2017. The Inversion Structures and Their Genetic Mechanisms of Bayindulan Sag, Erlian Basin. Earth Science, 42(4): 559-569. doi: 10.3799/dqkx.2017.044

Citation:

Chen Shuguang, Zhang Yiming, Cui Yongqian, Xiao Yang, Qin Fengqi, Lü Desheng, Zu Zhiyong, Li Yong, 2017. The Inversion Structures and Their Genetic Mechanisms of Bayindulan Sag, Erlian Basin. Earth Science, 42(4): 559-569. doi: 10.3799/dqkx.2017.044

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The Inversion Structures and Their Genetic Mechanisms of Bayindulan Sag, Erlian Basin

doi: 10.3799/dqkx.2017.044

1.
Geophysical Exploration Research Institute, Huabei Oilfield Company, PetroChina, Renqiu062552, China
2.
College of Geosciences, China University of Petroleum Beijing, Beijing102249, China

Received Date: 2016-10-22
Publish Date: 2017-04-15

Abstract

Abstract

The Geologic structure of Erlian basin has been controversial. To make clear the developmental periods of inversion structure and their genetic dynamic mechanism of Bayindulan sag, Erlian basin in Early Cretaceous, we make use of the new processing of 3D seismic data covering the all sag to identify the important tectonic unconformity interfaces and to make sure the contact relationship between the strata developed in Early Cretaceous. Combined the igneous rock revealing in drilling data, we think that the late 3^rd Member of K₁ba Formation, and the late 4^th member of K₁ba Formation, the late K₁bt₁, and the late K₁bt₂ mainly all developed normal inversion structures. The further studies indicate that the four positive inversion structures in the Early Cretaceous were caused by the developing magmatic diapiric structure under the setting of the regional extensional stress field; while inversion structure in early K₁bt₂ was typically caused by the regional strike-slip movement. Therefore, the genetic mechanisms of various inversion structures developed in different periods are dissimilar, which was closely coordinated with the subduction of Paleo-Pacific plate to Eurasia, the effects of the magmatic diapiric caused by the metasomatic mantle and regional strike-slip action resulted by the change of subduction direction of Paleo-Pacific plate during the Early Cretaceous period.
- Bayindulan sag,
- Early Cretaceous,
- inversion structure,
- genetic mechanism,
- petroleum geology

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References(61)

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The Inversion Structures and Their Genetic Mechanisms of Bayindulan Sag, Erlian Basin

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