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夕卡岩型铜矿床是长江中下游成矿带的一大特色,在我国占有重要位置,有必要进行深入的研究. 夕卡岩型铜矿床就其产出特征,可以分为三个亚型,即产于接触带上的正夕卡岩型、交代有利层位的层控夕卡岩型、沿断裂分布的隙控夕卡岩型. 笔者认为,伏牛山铜矿床属于隙控夕卡岩型矿床. 伏牛山夕卡岩型铜矿床地质特征伏牛山夕卡岩型铜矿床位于宁镇山脉中段,江宁县伏牛山南山地段.矿床赋存于伏牛山石英闪长岩体南侧外接触带五通组至龙潭组地层中.地层在褶皱过程中发生倒转,老地层盖在新地层
The skarn-type copper deposit is a major feature of the metallogenic belt in the middle and lower reaches of the Yangtze River, and occupies an important position in our country, so it is necessary to carry out further studies. The skarn-type copper deposit can be divided into three Subtype, that is produced in the contact zone of the positive skarn type, accountable the favorable stratigraphic control skarn type, along the fracture distribution skarn type .I believe that the Funiu Shan copper deposit belongs to the gap control Skarn deposit .Fu Niu Shan Skarn copper deposit geological characteristics Funiu Shan Skarn copper deposit is located in the middle of Ningzhen Mountains, Jiangning Funiu Shan Nanshan. Deposits occur in the Funiu Shan quartz diorite body On the south side, the Wutong Formation to the Longtan Formation strata contact the strata, and the strata are inverted during the folding process, with the old strata overlying the new strata