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江西地处环太平洋金属成矿带的外带,跨越两个大地构造单元:赣北属扬子准地台区;赣中及赣南属华南加里东褶皱区。元古代以来,两区均经历了多次强烈的构造运动(或地壳运动)和不同的大地构造发展阶段,因而,沉积建造、岩浆活动、构造形变和成矿作用极为复杂,矿产资源甚为丰富,为我国铜钨矿产资源基地之一。进一步研究和探讨江西地质构造的基本特征和铜铅锌成矿规律,为今后进一步开展铜铅锌的普查找矿具有一定的现实意义。
Jiangxi is located on the outskirts of the Pacific Rim Metallogenic Belt and spans two tectonic units: the sub-area of Yangtze in Jiangxi; the Central and South Caledonian fold areas in Jiangxi and Central Jiangxi. Since the Proterozoic, both regions experienced many intense tectonic movements (or crustal movements) and different stages of geotectonic development. Therefore, sedimentary construction, magmatism, tectonic deformation and mineralization are extremely complex with rich mineral resources , China’s copper and tungsten mineral resources base. Further study and discussion on the basic characteristics of geological structure and the laws of copper, lead and zinc mineralization in Jiangxi Province have certain practical significance for further prospecting for copper, lead and zinc in the future.