摘要
湘潭子金矿床处于秦祁昆造山系秦岭弧盆商丹蛇绿混杂岩带,中北秦岭加里东、燕山期铅锌、金、铜、银、锑、钼成矿带(Ⅲ-10),葡萄园-两当金、铅锌成矿带(Ⅳ21)。区内圈定矿带3条,金矿(化)体48条,为变质-热液型金矿床。
Xiangtanzi gold deposit is located in Shangdan OPHIOLITIC MELANGE belt of Qinling arc basin of Qinling orogenic system, Caledonian and Yanshanian lead-zinc, gold, copper, silver, antimony and molybdenum metallogenic belt(Ⅲ-10), Vineyard-Liangdang gold and lead-zinc metallogenic belt(Ⅳ-21). Three ore belts and 48 gold ore bodies are delineated in this area, which are metamorphic-hydrothermal gold deposits.
引文
[1]魏居珍.西秦岭太阳寺金矿地质地球化学特征及成因探讨.《长安大学硕士论文》.2018-05-02.
[2]刘学霖.甘肃两当县湘潭子金矿成矿流体研究.《中国地质大学(北京)硕士论文》.2018-05-01.
[3]胡晓隆.对北秦岭太阳寺矿集区金矿成矿特征的初步认识.《甘肃地质》.2008-03-15.