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南岭地区是中国最重要的有色金属、稀有金属成矿省,包括湘南、赣南、桂东、广东、福建,总面积达550000 km~2,以富产钨、锡著称于世。本文重点探讨本区中生代陆内造山的深部构造过程(作用)和地球物理特征及其对形成超巨量金属堆积的重要意义。南岭金属成矿省的构造演化可分为前寒武纪扬子板块和华夏板块的克拉通化、两板块消减的陆间造山及太平洋板块向洋壳消减的大陆活化3个阶段。笔者提出了表壳的“行—列—汇”控矿模式。据地震、地温和地电测量,认为本区从深
Nanling is the most important nonferrous metal and rare metal mineralization province in China, including southern Hunan, southern Jiangxi, eastern Guangxi, Guangdong and Fujian with a total area of 550000 km ~ 2. It is famous for its rich tungsten and tin production. This paper focuses on the deep tectonic processes and geophysical characteristics of the Mesozoic intracontinental orogen and its significance for the formation of massive deposits of metals. The tectonic evolution of the Nanling metallogenic province can be divided into three stages: the Precambrian Yangtze Plate and the Huaxia Plate, the cratonization of the plate, the reduction of interplateal orogeny between the two plates and the reduction of the Pacific Plate to the oceanic crust. I made the case of the “line - Column - Meeting” control mode. According to the earthquake, geothermal and geoelectric measurements, that the area from the deep