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雁林寺金矿是湖南有色地质勘查局90年代初在湘东北所发现的中型金矿床。它位于扬子地块东南缘,属于江南古陆金成矿带中段的湘东北金成矿区。1区域成矿背景湘东北地区位于扬子板块和华夏板块的结合部位,经历了复杂多期次的构造演化、岩浆活动以及深部热液或其他循环流体的运移过程。
Yanlin Temple Gold is a non-ferrous geological prospecting Bureau of Hunan Province in the early 90s found in the northeast of Hunan medium-sized gold deposits. It is located in the southeastern margin of the Yangtze block and belongs to the gold-bearing area in northeastern Hunan in the middle section of the gold mineralization belt of the Jiangnan Old Lu. REGIONAL METALLOGENIC BACKGROUND Northeastern Hunan is located at the junction of the Yangtze Plate and the Huaxia Plate, undergoing complicated multi-stage tectonic evolution, magmatic activity and migration of deep hydrothermal fluids and other circulating fluids.