摘要
柳林汊金矿区于扬子板块江南地轴南缘雪峰山成矿带典型的金矿床之一,本文对柳林汊金矿的矿区地质特征、矿体特征进行了介绍,认为该矿床应属于中-低温热液型金矿床,受地层、褶皱构造和热液蚀变的共同控制,并从构造、蚀变、地层、民采点等方面总结了其找矿标志。
The Liulincha gold deposit,located within Xuefeng mountain metallogenic belt in the southern margin of the Yangtze plate,is a typical gold deposit.In this paper,the author described the characteristics of the ore filed and the ore body,regard the deposit as low temperature hydrothermal gold deposits.The development of the deposit was controlled by the Madiyi formation,fold structure and hydrothermal alterations.The author also summarized ore-prospecting criteria of the deposit.
作者
张俊岭
ZHANG Jun-ling(Hunan Xinrui mining co.LTD of China Gold Group,Huaihua 419600,China)
出处
《世界有色金属》
2019年第21期60-61,共2页
World Nonferrous Metals
关键词
矿床特征
找矿标志
柳林汊金矿
雪峰山成矿带
扬子板块
deposit characteristics
prospecting signs
liulincha gold deposit
xuefengshan metallogenic bel
yangtze plate
