中国东北地区的构造格局与盆地演化

doi:10.11743/ogg20090502

Abstract

Abstract:

The Northeast China is not a Hercynian folded metamorphic belt(or orogenic belt),but a compound terrain pieced together after the Early Carboniferous.We name it "Jiamusi-Xingmeng Terrain".The Upper Paleozoic is not the crystalline basement for Meso-Cenozoic basins in Northeast China,but marine and continental sedimentary cover of para-caprock nature.The Late-Paleozoic marine sequences have well-developed dark mudstones and carbonates,which is the evidence for hydrocarbon potential.These sequences are important new targets for exploring oil and gas in Northeast China.We propose that the Meso-Cenozoic basins in Northeast China could be divided into three basin groups-the west,the middle and the east separated by the Jiayin-Mudanjiang fault and the Nenjiang-Kailu fault.The genetic type,characteristics of petroleum geology and the temporal and spatial evolution pattern of each basin are also discussed in this paper.

Key words: new sequence for oil and gas, basin group, Late Paleozoic, Jiamusi-Xingmeng terrain, Northeast China

CLC Number:

TE122.3

Zhou Jianbo, Zhang Xingzhou, Ma Zhihong, Liu Li, Jin Wei, Zhang Meisheng, Wang Chengwen, Chi Xiaoguo. Tectonic framework and basin evolution in Northeast China[J]. Oil & Gas Geology, 2009, 30(5): 530-538.

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Tectonic framework and basin evolution in Northeast China

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