黄骅坳陷孔南地区古近纪构造-地层格架和幕式演化过程

叶琳; 张俊霞; 卢刚臣; 张振宇

doi:10.3799/dqkx.2013.037

Volume 38 Issue 2

Mar. 2013

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YE Lin, ZHANG Jun-xia, LU Gang-chen, ZHANG Zhen-yu, 2013. Paleogene Structure-Stratigraphic Framework and Multiple Episode Evolution in Kongnan Area, Huanghua Depression. Earth Science, 38(2): 379-390. doi: 10.3799/dqkx.2013.037

Citation:

YE Lin, ZHANG Jun-xia, LU Gang-chen, ZHANG Zhen-yu, 2013. Paleogene Structure-Stratigraphic Framework and Multiple Episode Evolution in Kongnan Area, Huanghua Depression. Earth Science, 38(2): 379-390. doi: 10.3799/dqkx.2013.037

Citation:

YE Lin, ZHANG Jun-xia, LU Gang-chen, ZHANG Zhen-yu, 2013. Paleogene Structure-Stratigraphic Framework and Multiple Episode Evolution in Kongnan Area, Huanghua Depression. Earth Science, 38(2): 379-390. doi: 10.3799/dqkx.2013.037

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Paleogene Structure-Stratigraphic Framework and Multiple Episode Evolution in Kongnan Area, Huanghua Depression

doi: 10.3799/dqkx.2013.037

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan430074, China
2.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan430074, China
3.
Faculty of Economics and Management, China University of Geosciences, Wuhan430074, China
4.
Dagang Sub-Division of GRI, BGP, Tianjin300280, China

Received Date: 2012-09-15
Publish Date: 2013-03-01

Abstract

Abstract

Based on the newly released 3D seismic and drilling data in the Kongnan Area, Huanghua Depression, we tracked several sequence boundaries on the seismic profiles and interpreted structure styles and seismic reflection characteristics, which will help us identify an important tectonic unconformity boundary(Ek₁^Ⅲ) and further classify the episodic stages of tectonic evolution in Paleogene and build up structure-stratigraphic framework in rifting stages of the basin. Furthermore, we analyzed the detailed tectonic evolution processes of the basin with different tectonic episodes of rifting stages by means of backstripping and fault properties, combination types, activity analysis, that confirm that Ek₁^Ⅲ boundary represents the tectonic revolutionary boundary which imply a rifting initiation from upper First member of Kongdian Formation to Dongying Formation in Kongnan Area. From Third member of Kongdian Formation to lower First member of Kongdian Formation evolution of the basin was controlled by sag effect. At rifing stage, the basin underwent processes from extensional episode to dextral strike-slip and extensional episode.Both of the fault systems and subsidence center have migrated regularly and restricted the distribution of the basin depositional system.
- Huanghua Depression,
- Kongnan area,
- tectonic revolution,
- structure-stratigraphic framework

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References(48)

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Paleogene Structure-Stratigraphic Framework and Multiple Episode Evolution in Kongnan Area, Huanghua Depression

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