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著名的青藏滇缅印尼歹宇型构造出现于中国西部及东南亚面临印度洋地区。对于它的认识自一九二九年李四光教授首次提出来,随着各种地质资料的积累和研究的深入,已经大为充实与发展。近年来由于在该构造体系中以玉龙、当曲为代表的许多铜、铁矿产地的相继发现,并在此基础上对滇西川西藏东铜矿带和“三江四省(唐古拉)铁矿带”的圈定,人们越来越感觉到它的重要意义;加之板块学说出现以后,青藏高原及有关地区的地质构造特征及其发展历史,便成为大家所关心的一项课题。现在各路劲旅云集,以普查找矿为中心的地质战役已经打响,阵势正在铺开,在这种大好形势
The well-known Qinghai-Tibet, Burma and Indonesia-type structures appear in the Indian Ocean region in western China and Southeast Asia. For its understanding since Professor Li Sikuang first proposed in 1929, with the accumulation of various geological data and in-depth research has been greatly enriched and developed. In recent years, due to the successive discoveries of many copper and iron deposits represented by Yulong and Dangqu in this structural system, and on the basis of these discoveries, the eastern Yunnan copper belt and the “Three Rivers and Four Provinces (Tanggula) iron mines With ”" delineation, people feel more and more of its significance; combined with plate theory appears, the Qinghai-Tibet Plateau and related areas of geological structure and its development history, has become a subject of concern. Now all walks of life gathered in a row, to census prospecting geological campaign has been started, the battle is being rolled out in this excellent situation