青海省东昆仑东段区域成矿地质特征及地质背景浅析
|
摘要
东昆仑东段地处中国大陆中央造山带西段的东昆仑加里东造山带东段,是我国重要的矿产资源基地,该区经历了非常复杂的地质演化历史,发育有明显的构造特征,为区内成矿提供了非常有利的条件该区矿产资源相当丰富,尤其是金属矿产资源具有显著的地位。找矿潜力巨大。本文主要对该区地质特征与地质背景进行分析,希望为相关工作提供参考。
The East Kunlun orogenic belt in the eastern section of East Kunlun is located with the western part of the Central Orogenic China continent,is an important mineral resource base in China,the area has experienced a very complex geological evolution history,the development of structural characteristics,for ore-forming mineral resources in this region provide a very favorable condition is very rich especially,the metal mineral resources has significant status.Great prospecting potential.This paper mainly analyzes the geological features and geological background of the area,hoping to provide reference for related work.
The East Kunlun orogenic belt in the eastern section of East Kunlun is located with the western part of the Central Orogenic China continent,is an important mineral resource base in China,the area has experienced a very complex geological evolution history,the development of structural characteristics,for ore-forming mineral resources in this region provide a very favorable condition is very rich especially,the metal mineral resources has significant status.Great prospecting potential.This paper mainly analyzes the geological features and geological background of the area,hoping to provide reference for related work.
引文
[1]赵双喜.青海东昆仑中段金铜资源远景评价报告.2013,(10).
[2]陆松年.青藏高原北部前寒武纪地质初探,地质出版社.2012,32(12).
[3]崔廷军,逯克思,庄勇,等.青海省柴达木盆地南缘金成矿带特征及成矿规律浅析[J].黄金科学技术,2010(3):63-67.
[4]田承盛.东昆仑中段五龙沟矿集区金矿成矿作用及成矿预测研究[D].北京:中国地质大学,2012.(10).
[5]高珍权.东天山铜金多金属成矿学及找矿系统工程学[D].中南大学,2012.
[2]陆松年.青藏高原北部前寒武纪地质初探,地质出版社.2012,32(12).
[3]崔廷军,逯克思,庄勇,等.青海省柴达木盆地南缘金成矿带特征及成矿规律浅析[J].黄金科学技术,2010(3):63-67.
[4]田承盛.东昆仑中段五龙沟矿集区金矿成矿作用及成矿预测研究[D].北京:中国地质大学,2012.(10).
[5]高珍权.东天山铜金多金属成矿学及找矿系统工程学[D].中南大学,2012.