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湘西花垣矿集区位于扬子地块东南边缘与雪峰(江南)造山带的过渡部位,构造上位于NE向湘黔断裂带中部,经历了晋宁期碰撞造山、加里东期拉张裂陷-被动大陆边缘盆地-前陆盆地以及印支期-燕山期陆内变形等演化过程,形成了多种沉积/层控金属矿产和非金属矿产,是湘西-鄂西成矿带的重要组成部
The Huayuan ore district in western Hunan is located at the transitional part between the southeastern edge of Yangtze block and the Xuefeng (Jiangnan) orogenic belt. It is located in the middle of NE-Xiang-Qian fault zone and experienced the Jinning period collision orogeny, Caledonian tensile- In the evolution of the inland continental margin-foreland basin and Indosinian-Yanshanian intracontinental deformation, a great deal of sedimentary / stratabound metallogenic and nonmetallic minerals are formed, which is an important part of the western Hunan-Hubei region metallogenic belt