喜马拉雅和青藏高原深剖面研究的进展  

THE PROGRESS OF DEEP PROFILING STUDY IN HIMALAYA AND QINGHAI─XIZANG (TIBET) PLATEAU

作　　者：赵文津[1] 黄立言[1] 熊嘉育[1] 

机构地区：[1]中国地质科学院,北京100037

出　　处：《地球物理学报》1997年第S1期140-152,共13页Chinese Journal of Geophysics

摘　　要：概述了1992─1996年中、美、德合作开展“喜马拉雅和青藏高原深剖面及综合研究”的主要进展，包括研究项目的提出、工作进展概况和取得的主要科学、技术成果；并对今后的工作提出了建议．The principal progresses of the “International Deep Profiling of Tibet and Himalaya”conducted jointly by Sino-US-German scientists during 1992─1996 are outlined in this paper, including the advancement of the project, the brief account of the study and the principal scientific-technical results obtained, with some considerations and suggestions toward the INDEPTH-Ⅲ also put forward.

关 键 词：喜马拉雅 青藏高原 深剖面 主喜马拉雅逆冲断裂 过江反射带 熔融层 

分 类 号：P56[天文地球—构造地质学]