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Objective The widely-distributed reformed basins in China are currently major areas for oil and gas exploration.Post-stage tectonic movement of modified basins often plays an important role in controlling petroleum accumulation,migration and distribution(Liu and Yang,2000).The petroliferous Carboniferous-Permian Yingen-Ejinaqi Basin is located in the junction area between the North China Craton and the Central Asian Orogenic Belt(Fig.la),which has experienced multiple tectonic reformation events since the late Paleozoic.Limited by a lack of sedimentary records and harsh natural conditions,the timing and duration of the tectonic reformation events remain unclear.In this study,we performed detrital apatite fission-track(AFT)and zircon U-Pb(ZUPb)chronology,in order to investigate the reformation processes of the eastern Yingen-Ejinaqi Basin.This study benefits the understanding of tectonothermal history for further petroleum exploration in the Yingen-Ejinaqi Basin.
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篇名 Discovery of Multiple Tectonic Reformations of the Eastern Yingen-Ejinaqi Basin:Evidence from Detrital Chronology
来源期刊 地质学报(英文版) 学科
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年,卷(期) 2021,(2) 所属期刊栏目 RESEARCH ADVANCES
研究方向 页码范围 693-695
页数 3页 分类号
字数 语种 英文
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地质学报(英文版)
双月刊
1000-9515
11-2001/P
16开
北京复外百万庄26号
1922
eng
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3189
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