摘要
本文所研究的青海省那更康切尔地区位于秦祁昆造山系—东昆仑弧盆系—北昆仑岩浆弧带,具有强烈的岩浆活动,且地层因受构造和岩体影响,构造带作为混杂岩带,内有许多折裂块体和岩石碎片,具备了造山层构造特征,所以其在含矿地质的勘探和研究中有很大价值。
The nagen Kangqi area in Qinghai Province studied in this paper is located in the qinqikun Orogenic System East Kunlun arc basin system North Kunlun magmatic arc belt,which has strong magmatic activity,and the stratum is affected by the structure and rock mass.As a melange belt,the structural belt has many fractured blocks and rock fragments,which has the structural characteristics of orogenic layer,so it is in the exploration and research of ore bearing geology It has great value.
作者
马生福
MA Sheng-fu(Qinghai natural resources Museum,Xining 810000,China)
出处
《世界有色金属》
2019年第22期98-99,共2页
World Nonferrous Metals
关键词
青海省
银多金属矿床
矿石矿物特征
地质意义
qinghai province
silver polymetallic deposit
ore mineral characteristics
geological significance