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区域地球化学特征及其主控因素——对内蒙古珠斯楞地区找矿的意义
引用本文:王嘉伟,李小强,陈清石,牛广智.区域地球化学特征及其主控因素——对内蒙古珠斯楞地区找矿的意义[J].地质通报,2016,35(9):1544-1549.
作者姓名:王嘉伟  李小强  陈清石  牛广智
作者单位:1. 陕西区域地质矿产研究院, 陕西 咸阳 712000;2. 长安大学, 陕西 西安 710054
基金项目:中国地质调查局项目(编号:1212011085091)
摘    要:在1∶5万水系沉积物测量的基础上,对内蒙古额济纳旗珠斯愣地区的地球化学特征及其主控因素进行初步分析,并对元素分布特征、元素相关性分析、单元素异常与构造之间关系、综合异常与构造之间关系进行了探讨。研究发现,Cu、Au、Sb为区内具一定潜力的找矿元素,与呼伦西白-珠斯楞海尔罕反"S"形构造带南端内、外旋面的转换的珠斯楞海尔罕一带形成一个与断裂构造吻合度较高的、半环性的成矿成晕中心。因而推断,区内具有形成与中酸性侵入岩有关的热液铜多金属矿的可能,其中珠斯楞海尔罕铜金矿和道布青乌苏南北金锑矿2个找矿靶区严格受呼伦西白-珠斯楞海尔罕反"S"形构造的控制。

关 键 词:水系沉积物测量  找矿靶区  珠斯楞地区
收稿时间:2016/4/21 0:00:00
修稿时间:2016/6/27 0:00:00

Regional geochemical characteristics and main control factors: Prospecting significance in Zhusileng area, Inner Mongolia
WANG Jiawei,LI Xiaoqiang,CHEN Qingshi and NIU Guangzhi.Regional geochemical characteristics and main control factors: Prospecting significance in Zhusileng area, Inner Mongolia[J].Geologcal Bulletin OF China,2016,35(9):1544-1549.
Authors:WANG Jiawei  LI Xiaoqiang  CHEN Qingshi and NIU Guangzhi
Institution:1. Academy of Regional Geological Survey and Mineral Resources Exploration of Shaanxi, Xianyang 712000, Shaanxi, China;2. Chang''an University, Xi''an 710054, Shaanxi, China
Abstract:On the basis of 1:50000 stream sediment survey, the authors made a preliminary analysis of the geochemical characteristics and main control factors of Zhusileng area in Inner Mongolia. The relationship of element distribution, element correlation analysis and single element anomaly to structure and the relationship between the anomaly and structure were investigated. It is found that Cu, Au, and Sb are potential prospecting elements in this area, which form a half-ring ore-forming and halo-forming center in relatively high accord with the fault structure in the converting Zhusilenghaierhan zone of inner and outer spiral surface at the south end of reverse "S" structure of Hulunxibai-Zhusilenghaierhan. Therefore, it is concluded that there may be hydrothermal copper polymetallic ore deposit related to the formation of intermediate-acidic intrusive rocks, where the gold deposit in Zhusilenghaierhan and two gold-antimony prospecting targets respectively in southern and northern Daobuqingwusu are strictly controlled by reverse "S" structure of Hulunxibai-Zhusilenghaierhan.
Keywords:stream sediment survey  prospecting target  Zhusileng area
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