首页> 中文期刊> 《中国锰业》 >准噶尔盆地南缘霍玛吐背斜带构造演化分析

准噶尔盆地南缘霍玛吐背斜带构造演化分析

         

摘要

霍玛吐背斜带位于准噶尔盆地北天山的山前冲断带,拥有良好的石油地质条件,大地构造位置比较复杂,受晚古生代以来的海西、印支、燕山和喜山多期次(或同期次)不同构造体系的叠加与复合,形成众多的圈闭,发育规模和时空展布等具有多期性、多样性和复杂性等特点,油气苗显示活跃,资源量大.其中,霍-玛-吐构造带是准南规模最大的一排构造单元,具有良好油气勘探前景.%HuoMaTu anticline belt is located in the piedmont thrust belt of southern margin of Junggar basin with good petroleum geological conditions.Its tectonic position is more complex with the superposition and recombination of different tectonic systems in the Hercynian days, including Indosinian, Yanshan and Himalayan periods since late Paleozoic times.A large number of traps are formated, as has the characteristics of multiphase nature, diversity and complexity in the development scale and space-time distribution and so on.There is active seepage and large amount of resources.Among them, the Huoerguosi-Manasi-Tugulu structure belt is the largest structural unit, and it has favorable foreground of exploration.

著录项

相似文献

  • 中文文献
  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号