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贵州遵义锰矿国家整装勘查区位位于扬子地块东南缘的武陵山成矿带中段。著名的二叠纪茅口晚期遵义锰矿,形成于华南地块裂解背景下的水城—遵义台沟中。近年来,项目团队在该区通过长期的产学研协同攻关,找到了遵义锰矿底板“白泥塘层”硅质岩的热水成因证据,详细梳理了锰矿成矿的构造古地理背景,发现了遵义锰矿的矿床类型——海底喷流沉积型锰矿床。通过该整装勘查区的实践检验,先后新发现大型锰矿床2个(深溪锰矿、永安锰矿),中型锰矿床2个(小金沟锰矿、转龙庙锰矿),新发现的锰矿资源量,超过了以往保有资源量的两倍,实现了遵义锰矿找矿的重大突破。根据成矿预测,遵义锰矿找矿潜力依然巨大。
The Zunyi Manganese Mine in Guizhou Province is located in the middle of the Wulingshan metallogenic belt at the southeastern margin of the Yangtze block. The famous Permian Maokou Zunyi manganese deposit, which was formed in the Shuicheng-Zunyi Trench Valley under the cracking of South China block. In recent years, the project team in the area through long-term collaborative research with production and research to find the Zunyi manganese basement “white mud layer ” chert of hot water genesis evidence, a detailed carding of the manganese mineralization of tectonic paleogeographic background and found that The Zunyi manganese deposit type - submarine jet sedimentary manganese deposit. Through the practice test of the integrated exploration area, two newly discovered large-scale manganese deposits (Shenxian Manganese Mine and Yongan Manganese Mine) and two medium-sized manganese ore deposits (Xiaoguogou Manganese Mine and Zhuanlongmiao Manganese Mine) have been newly discovered. Newly discovered manganese ore resources, More than twice the amount of resources held in the past, and achieved a major breakthrough in the prospecting of Zunyi manganese ore. According to mineralization prediction, Zunyi manganese ore prospecting potential is still huge.