苏北-南黄海南部叠合盆地构造演化与海相油气勘探潜力

doi:10.11743/ogg20070105

Abstract

Abstract:

Based on comprehensive study on tectonic stress field,structural feature,and sedimentary formation,the tectonic evolution of Subei-South Nanhuanghai(North Jiangsu-Southern South Yellow Sea) superimposed basin since the late Triassic plate collision between the Huanan plate and Huabei plate can be divided into the following four stages: ① the foreland basin development stage under the influence of the late Triassic to Middle Jurassic paleo-Tethyan closing;② the thrust nappe development stage controlled by the Late Jurassic-Early Cretaceous oblique subduction of Izanagi oceanic plate;③ the basin extension development stage under the in-fluence of the late Cretaceous-Paleogene subduction of the Pacific plate,including the late Cretaceous depression development stage and Paleogene fault depression basin development stage;④ the depression development stage under the influence of Neogene Himalaya orogenesis.In relation to the development of the Paleogene half-graben-like fault depression,this paper focuses on the controlling effects of the left-lateral strike-slip and pul-lingapart movement along with the NWW basement faults and of the NE thrust nappe over the development of the basin and half graben-like fault depression,and points out the exploration prospect of marine petroleum system from the aspect of sedimentation,reworking,and preservation.

Key words: superimposed basin, tectonic evolution, marine sequence, petroleum system, late-formed hydrocarbon accumulation, Subei-South Nanhuanghai, South China

CLC Number:

TE111.1

Ma Liqiao, Chen Hanlin, Dong Yong, Xia Jiufeng, Sun Fengxia, Yang Lanying. Tectonic evolution of Subei-South Nanhuanghai superimposed basin from the Late Mesozoic to the Cenozoic and marine petroleum potential[J]. Oil & Gas Geology, 2007, 28(1): 35-42.

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Tectonic evolution of Subei-South Nanhuanghai superimposed basin from the Late Mesozoic to the Cenozoic and marine petroleum potential

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