Formation and tectonic evolution of Laoshan uplift of South Yellow Sea basin and its effect on hydrocarbon accumulation

CHEN Chunfeng; SHI Jian; XU Donghao; ZHANG Yinguo; ZHANG Bocheng; WANG Jun

doi:10.16562/j.cnki.0256-1492.2018.03.005

Marine Geology & Quaternary Geology > 2018 > 38(3): 55-65. > DOI: 10.16562/j.cnki.0256-1492.2018.03.005

CHEN Chunfeng, SHI Jian, XU Donghao, ZHANG Yinguo, ZHANG Bocheng, WANG Jun. Formation and tectonic evolution of Laoshan uplift of South Yellow Sea basin and its effect on hydrocarbon accumulation[J]. Marine Geology & Quaternary Geology, 2018, 38(3): 55-65. DOI: 10.16562/j.cnki.0256-1492.2018.03.005

Citation:

Formation and tectonic evolution of Laoshan uplift of South Yellow Sea basin and its effect on hydrocarbon accumulation

1.
Shanghai Branch of CNOOC Ltd., Shanghai 200335, China
2.
Institute of Geophysics and Geomatics, China University of Geosciences(Wuhan), Wuhan 430074, China
3.
Qingdao Institute of Marine Geology, CGS, Qingdao 266071, China

More Information

Received Date: January 30, 2018
Revised Date: April 01, 2018

Graphical Abstract

Abstract

Abstract

Based on the newly acquired drilling data and seismic data, comprehensive study has been devoted to the stratigraphic and tectonic evolution of the Mesozoic-Paleozoic on the Laoshan uplift in the South Yellow Sea Basin, and comparison is made with southern Jiangsu Province and western Zhejiang Province in the land area of the Lower Yangtze platform. It is revealed that there are two depositional stages, the first stage from late Sinian to early Ordovician, and the second stage of early Triassic, dominated by carbonate platform deposits consisting of limestone and dolomite, while deep water deposits of mudstone and argillaceous limestone occur in the western Zhejiang Province. During the period from Late Ordovician to Silurian, tectonic movement became intensified. The Laoshan uplift rose as a whole in Mesozoic and Cenozoic. At the same time, thicker dolomite reservoirs were formed, which provided large space for hydrocarbon accumulation. The uplift formed in the early stage favored the migration of hydrocarbons upwards from the deep water basin or aulacogen and finally accumulated in the traps of the uplifted area.
- South Yellow Sea Basin,
- Laoshan uplift,
- formation,
- structural evolution,
- hydrocarbon accumulation

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References (25)

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