• 责任者：Chen Yuan (College of Resources and Environment ; Southwest Petroleum University ; Chengdu 610500 ; China) ; Mou Zhonghai
• 刊名：Fault-Block Oil and Gas Fields
• 出版年：2012
• 卷期：19(4)
• 关键词：盆山耦合 ; basin range coupling ; 构造演化 ; structural evolution ; 柴达木盆地 ; Qaidam Basin
• 页码：p.414-417
• 图表：1 illus., 24 refs.
• 分类号：0300
• issnNo：ISSN1005-8907
• isbnNo：CN41-1219/TE

According to the research of seismic profile contrast and outcrop data in the western Qaidam Basin, it is believed that the relationship between basin and mountain presents a great difference in different regions and different periods in the study area. The contact relationship between Altun Mountains and basin is mainly the fault contact and overlap contact. Contact pattern in the northern part of Hong Gouzi Area shows a lower-fault and upper-overlap type. Typical half-flower fault contact presents in the area of Yueya Mountains, and overlap control relationship appears in Hong Guuzi and in the western parts of oil. The contact pattern between Kunlun Mountains and basin shows the normal fault contact in Mesozoic, but the contact pattern shows the overlap contact in Alar and Futou Mountains region. Basin-mountain pattern is mainly thrust fault contact in Cenozoic. Right-lateral strike-slip fault contact is between the middle-western part and eastern part in front of Kunlun Mountains.