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《Journal of Beijing Polytechnic College》 2011-03
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Foreland basin and its sedimentary response to the fold-thrust belt

Ding Wenjun1 Sun Luo1 Guan Bo1 Jiang Qi1 Li Zhihui2(1.Beijing Polytechnic College,Beijing 100042,China;2.Beijing Jiangong Architectural Design Institute,Beijing 100024,China)  
A foreland basin generally is defined as an elongate basin that forms between a linear contractional orogenic belt and the stable cration,mainly in response to flexural subsidence that is driven by thrust-sheet loading in the orogen.It is an ideal place to investigate the coupling between the basin and the mountain and to explore the prospect for oil and gas.Here we review the definition,characteristics,classification of the foreland basin in details.Based on the synthesis of two kinds of typical foreland basin,we propose that the following signatures be ulitized to recognize the sedimentary responses to the fold-thrust belt: unconformities,the appearance of conglomerate wedge,the migrations of subsidence,the changes of diagnostic clasts of sandstone and conglomerate,the uplift and migration of the forebulge.
【CateGory Index】: P542
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