• 责任者：Qu Shaodong (State Key Laboratory of Continental Dynamics ; Department of Geology ; Northwest University ; Xi’an 710069 ; China) ; Liu Chiyang
• 刊名：Chinese Journal of Geology
• 出版年：2013
• 卷期：48(1)
• 关键词：断裂带 ; fracture zones ; 油气聚集 ; oil and gas accumulation ; 松辽平原 ; Songliao Plain
• 页码：p.245-253
• 图表：illus., 30 refs.
• 分类号：0300
• issnNo：ISSN0563-5020
• isbnNo：CN11-1937/P

Based on our research, Qinjiatun fracture was composed by two right-lateral fractures, and formed in early Huoshiling period which controlled sedimentary thickness of the Huoshiling formation. While Qindong fracture formed relatively later,the major active stage is Denglouku- early Quantou period, which cut the early formed two right-lateral Qinjiatun fault, Qindong fault is a typical strike-slip fault. Qinjiatun fault and Qindong fault played a decisive role for the hydrocarbon migration and accumulation in this region.