摘要
大兴安岭南段位于贺根山断裂与西拉沐伦河断裂之间,发育了众多的多金属矿床,矿床以多种成矿元素共生、伴生为特点,其中铅、锌、银矿床占据了最为重要的地位,其与锡矿构成了统一的成矿系统,同时受到燕山晚期高演化花岗岩的制约,本文以白音诺尔-红岭地区为例,从赋矿地层、成矿系统、侵入岩等方面指出了该区锡多金属找矿的新方向。
Located between the Hegenshan fault and the Xilamulunhe fault,the Southern section of Daxinganling has developed a large number of polymetallic deposits.The deposits are characterized by the symbiosis and association of various metallogenic elements,among which the lead,zinc and silver deposits occupy the most important position.It forms a unified metallogenic system with tin ore and is constrained by the high-evolution granite in the late Yanshan period.This paper takes Baiyinnuo-Hongling area as an example,and points out the new direction of tin metal ore prospecting in the area from the aspects of mineralization strata,metallogenic systems,and intrusive rocks.
作者
徐巧
黄行凯
刘孜
祝新友
付水兴
XU Qiao;HUANG Xing-kai;LIU zi;ZHU Xin-you;FU Shui-xing(Beijing Institute of Geology for Mineral Resources,Beijing 100012)
出处
《世界有色金属》
2018年第10期113-114,共2页
World Nonferrous Metals
基金
中国地质调查局基础性公益性地质矿产调查项目(编号:DD20160072)
关键词
大兴安岭南段
锡多金属
找矿方向
Daxinganling South Section
Tin metal
Looking for mine direction
