位于青藏高原腹地的羌塘盆地是经历了多期构造改造的改造型盆地。
The Qiangtang Basin in the hinterland of the Qinghai-Xizang Plateau is interpreted as a reworked basin which has undergone multiple phases of tectonic reworking.
介绍了青藏高原羌塘盆地和措勤盆地的深部磁场特征，用隐伏裂陷槽的观点分析了这些特征。
The deep magnetic field characteristics in Qiangtang basin and Cuoqin basin of Qinghai-Ti-bet plateau is presented and analyzed by means of viewpoint of buried aulacogen.
介绍了青藏高原羌塘盆地和措勤盆地的深部磁场特征，用隐伏裂陷槽的观点分析了这些特征。
The deep magnetic field characteristics in Qiangtang basin and Cuoqin basin of Qinghai-Ti-bet plateau is presented and analyzed by means of viewpoint of buried aulacogen.
应用推荐