A STUDY OF THE GRAVITY FIELD ON THE NORTHERN MARGIN OF QINGHAI-TIBET PLATEAU
Meng Lingshun1, Qi li2, Gao Rui2, Guan Ye2
1. Changchun University of Science and Technology, Changchun 130026;
2. Research Center of Lithosphere, Chinese Academy of Geological Sciences, Beijing 100037
Based on the gravity field characteristics along Algan-Laomangya and Golmud Ejin Banner geoscience Transections as well as the relevant geological data, the authors have divided the study area into five second order tectonic units with eleven relatively large faults, calculated and analysed Airy isostatic anomalies and Moho depth. It is inferred that the Central Qilian fault in the Altun fold system is the northern boundary of Qinghai Tibet plateau.
孟令顺, 齐立, 高锐, 管烨. 青藏高原北缘重力场研究[J]. 物探与化探, 1998, 22(3): 183-190.
Meng Lingshun, Qi li, Gao Rui, Guan Ye. A STUDY OF THE GRAVITY FIELD ON THE NORTHERN MARGIN OF QINGHAI-TIBET PLATEAU. Geophysical and Geochemical Exploration, 1998, 22(3): 183-190.