• 责任者：Zhou Wen (State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Li Xiuhua
• 刊名：Acta Petrologica Sinica
• 出版年：2011
• 卷期：27(8)
• 关键词：碳酸盐岩油气藏 ; carbonate reservoir ; 断裂带 ; fracture zones ; 古岩溶 ; paleokarst ; 塔里木盆地 ; Tarim Basin
• 页码：p.2339-2348
• 图表：5 illus., 1 table, 22 refs.
• 分类号：1003
• issnNo：ISSN1000-0569
• isbnNo：CN11-1922/P

The analysis of systematic statistics of Ordovician fault characteristics in Tahe in this paper shows that the large karst caves most probably distributed in the caves which are below the boundary of T74 and mostly controlled by mid-large faults.According to the relationship between faults and the development of karst caves,the concepts of “fault which could control karst caves” and “fault which controlled by karst caves” have been proposed,and it is believed in this paper that middle-large faults in Tahe are mainly “fault which could control karst caves”,but the small fractures in this area are mostly “fault which controlled by karst caves”.On the basis of the theory of “fault which could control karst caves”,the mode of “fault-paleokarst” in Ordovician of Tahe area has been established.