首页> 中文期刊>地震工程学报 >从地球物理场信息分析西宁盆地地热地质条件

从地球物理场信息分析西宁盆地地热地质条件

     

摘要

Based on the comprehensive explanation of controllable source audio frequency geo-mag-netic sounding and previous geophysical prospecting data as gravity, earthquake, geo-magnetic sounding and direct current electric sounding, the tectonic framework of uplift with depression and features of Xining basin are obtained. According to distribution character of geothermal field, the geothermal reservoir type of Xining basin is discussed. It is indicated that the Xining depression in Xining basin is extensional and transtensile fault depression, characterized by higher geothermal field and geothermal gradient, it has both geothermal reservoir of fracture convection type and basin conduction type. While Datong and Pingan depression in Xining basin are compress-shear depressions, characterized by lower geothermal field and geothermal gradient, with reservior of basin conduction type. Xining depression is a favourable exploring region for geothermal resource.%在对西宁盆地进行可控源音频大地电磁测深(CSAMT)全面探测的基础上,结合以往重力、地震、大地电磁测深、直流电测深等物探资料综合解释,揭示了西宁盆地隆坳构造格局和盆地性状,据地温场分布特征探讨了热储类型,指出西宁盆地中西宁坳陷属张性、张扭性,具有地温场高、地温梯度大的特点,且热储类型具盆地传导兼断裂对流型特征;大通、平安坳陷属压性、压扭性坳陷,地温场、地温梯度相对较低,热储类型为盆地传导型.西宁断陷是地热开发有利地段.

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