阿尔金山及邻近地区深部地电结构探讨  

DEEP-SEATED GEOELECTRIC STRUCTURES IN THE ALTUN MOUNTAINS AND ITS NEIGHBOURING AREA

作　　者：鲁新便[1] 

机构地区：[1]西北石油地质局第一物探大队

出　　处：《新疆地质》1995年第3期256-263,共8页Xinjiang Geology

基　　金：国家重点科研攻关项目

摘　　要：探讨了阿尔金山、柴达木盆地、塔里木盆地的深部地电结构特征和各构造单元之间的地电接触关系。指出阿尔金隆起、柴达木和塔里木盆地地壳深部存在壳内高导层。塔里木盆地东南部和柴达木盆地百北部均存在规模较大的逆掩推覆构造，它们的形成、发展和阿尔金断裂系的构造演化密切相关。The characters are described of deep-seated geielectric structures in the Altun Mts.,Chaidamu basin and Tarim basin.The geoelectric contact of three units is also discussed. It is pointed that intracrust high-conductivity layers exist in the deep crusts of Altun uplift, Chaidamu basin and Tarim basin.Largesized thrusting nappes exist in the southeastern Tarim basin and northwestern Chaidamu basin, which are closely related with the tectonic evolution of Altun fault system.

关 键 词：阿尔金山 培里木 柴达木 深部地电结构 

分 类 号：P319[天文地球—固体地球物理学]