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通过近年来的研究 ,提出了全新的喜马拉雅构造 -成矿域概念。从大喜马拉雅构造域及其成矿效应出发 ,通过构造域对矿集区的控制作用、成矿时代、成矿物质来源、深部过程与成矿效应的分析 ,从而较全面地评价了青藏高原及邻区的资源潜力和需要进一步工作的重要成矿带或矿集区。通过分析认为喜马拉雅构造 -成矿域内强烈的壳幔物质交换 ,下地壳翻天覆地的物质和流体交换 ,导致了在同一构造地质单元内可以有一个或多个超大型矿床的存在。并对多个重要矿床类型提出了更切合实际的观点 ,如西藏甲马铜钼银铅锌金多金属矿床属于矽卡岩 -斑岩复合型 ,云南羊拉铜钼金多金属矿床也属于矽卡岩 -斑岩复合型矿床等。在喜马拉雅构造域内形成的燕山晚期或喜马拉雅期矿床大多和大陆地壳深部复杂的动力学过程有关 ,所形成的矿床矿物组合及成矿元素组合复杂 ,特别是矿石中钴、银元素含量较高 ,许多矿床中银、钴已经作为主要成矿元素。最后明确提出了青藏高原主体及东缘重要矿集区的资源潜力
Through the research in recent years, a new Himalayan tectonic-metallogenic domain concept has been proposed. Based on the tectonic domain of the Greater Himalaya and its metallogenic effect, through the control of tectonism, the metallogenic epoch, the source of metallogenic material, the deep process and the metallogenic effect, the tectonic domain of the Greater Himalayas and its metallogenic effect are comprehensively evaluated. Resource potential of adjacent areas and important metallogenic belt or ore gathering area that requires further work. By analyzing the strong exchange of crust-mantle material in the Himalayan tectonic-metallogenic domain, the earth-shaking exchange of materials and fluids in the lower crust led to the existence of one or more superlarge deposits within the same tectonic unit. And a number of important types of deposits put forward a more realistic point of view, such as the Tibet Jiama Cu-Mo-Ag-Pb-Zn-Au polymetallic deposits belong to skarn-porphyry complex type, Yunnan Yangla copper-molybdenum gold polymetallic deposits also belong to silicon Clay - porphyry complex deposits. Most of the late Yanshanian or Himalayan deposits formed in the Himalayan tectonism are related to complex deep-sea dynamic processes in the continental crust. The mineral assemblages and metallogenic element assemblages formed by the deposit are complex. In particular, the contents of cobalt and silver in the ore are high, many of which Deposit silver, cobalt has been as the main ore-forming elements. Finally, the potential of the main Qinghai-Xizang Plateau and the important ore-gathering areas in the eastern margin are clearly put forward