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新疆温宿峡谷盐底辟构造与油气聚集

王会萍

西安科技大学学报2011,Vol.31Issue(1):59-63,5.
西安科技大学学报2011,Vol.31Issue(1):59-63,5.

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

王会萍1

作者信息

  • 1. 长安大学,资源学院,陕西,西安,710054
  • 折叠

摘要

Abstract

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

天文与地球科学

引用本文复制引用

王会萍..新疆温宿峡谷盐底辟构造与油气聚集[J].西安科技大学学报,2011,31(1):59-63,5.

基金项目

国家自然科学(40172076) (40172076)

新疆维吾尔自治区区地质矿产调查项目(XJQDZ2004-12) (XJQDZ2004-12)

西安科技大学学报

OACSTPCD

1672-9315

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