新疆温宿峡谷盐底辟构造与油气聚集  

Ochirbat salt diapiric structure and hydrocarbon accumulation in the canyon of Xinjiang Wensu county

作　　者：王会萍[1] 

机构地区：[1]长安大学资源学院,陕西西安710054

出　　处：《西安科技大学学报》2011年第1期59-63,共5页Journal of Xi’an University of Science and Technology

基　　金：国家自然科学(40172076);新疆维吾尔自治区区地质矿产调查项目(XJQDZ2004-12)

摘　　要：盐底辟是分布最广泛的一种底辟构造。本文在展示奥奇克盐底辟构造的区域地质概况和空间形态的基础上,从规模和完整性方面,都证明它不愧是全国乃至全世界都是独一无二的典型代表,进而分析了其完整的演化过程和形成机制,全面显示了其重要的地质构造科考价值和地质遗迹保护观赏价值,最后提出新疆温宿峡谷盐底辟构造应该与其他盐底辟构造一样,可形成多种油气圈闭,是一种重要的油气储集构造。The salt diapiric structure has the most extensive distribution in all diapiric structures.On the basis of showing the condition of its area geology and the space pattern of the Ochirbat salt diapiric structure,the paper demonstrates that the Ochirbat salt diapiric structure is a seldom seen geological remains and is really a unique typical representative in China even in the world because of its completive and grand spatial pattern.Moreover,analyzes its total developing process and forming mechanism and replays its precious values of protection and appreciation in the fields of the science and investigation.Finally,put forward that the Ochirbat salt diapiric structure in the canyon of Xinjiang Wensu County can form many oil and gas trap and it＇s an important oil bearing structure.

关 键 词：奥奇克盐底辟构造 空间形态 形成机制 油气聚集 

分 类 号：P631.8[天文地球—地质矿产勘探]