晚震旦至中奥陶世下扬子被动大陆边缘原型盆地特征

印峰; 杨风丽; 叶芳; 吴哲; 吴满

doi:10.3799/dqkx.2013.103

Volume 38 Issue 5

Sep. 2013

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Article Navigation > Earth Science > 2013 > 38(5): 1053-1064

YIN Feng, YANG Feng-li, YE Fang, WU Zhe, WU Man, 2013. Late Sinian-Middle Ordovician the Prototype Basin Characteristics of Passive Continental Margin in Lower Yangtze. Earth Science, 38(5): 1053-1064. doi: 10.3799/dqkx.2013.103

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YIN Feng, YANG Feng-li, YE Fang, WU Zhe, WU Man, 2013. Late Sinian-Middle Ordovician the Prototype Basin Characteristics of Passive Continental Margin in Lower Yangtze. Earth Science, 38(5): 1053-1064. doi: 10.3799/dqkx.2013.103

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Late Sinian-Middle Ordovician the Prototype Basin Characteristics of Passive Continental Margin in Lower Yangtze

doi: 10.3799/dqkx.2013.103

YIN Feng^{1, 2
,},
YANG Feng-li^{2, 3},
YE Fang²,
WU Zhe²,
WU Man²

1.
SINOPEC Exploration Southern Company, Chengdu 610041, China
2.
School of Ocean and Earth Science, Tongji University, Shanghai 200092, China
3.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

Received Date: 2012-11-12
Publish Date: 2013-09-15

Abstract

Abstract

As the second oil and gas pioneering project progresses, marine strata has become the focus in the field of oil and gas exploration. Lower Yangtze has deposited thick marine strata, and its prototype basin has experienced structural transformation of multi-period times. This paper discusses the boundary under the Yangtze, aiming to conduct a systematic analysis of the entire system. Based on the "TSM" strategy of basin prototype analysis on the basin tectonics, deformation and sedimentary, the residual strata distribution from Late Sinian to Middle Ordovician in the Lower Yangtze and the sedimentary filling during the process are analyzed. The results indicate that the Lower Yangtze has evolved passive continental margin in the Late Sinian-Middle Ordovician, which is characterized mainly by siliceous classic sediments, carbonate sediment and synsedimentary faults, etc.. During this period, carbonate platform developed into trim platform. The platform had lateral growth phenomenon and the sediment of tongue protruding input to the sea basin. Jiangnan fault, a typical synsedimentary fault, shows that the source material of the sediment basin has always been transported from northwest to southeast by the internal one-way transportation in the Lower Yangtze. All these indicate that it was mature passive continental from the Late Sinian to Middle Ordovician.
- Lower Yangtze,
- prototype basin,
- passive continental margin,
- residual strata,
- sedimentation,
- hydrocarbons

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References(80)

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Late Sinian-Middle Ordovician the Prototype Basin Characteristics of Passive Continental Margin in Lower Yangtze

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