浩布高铅锌铜锡矿床地物化综合找矿模式探讨
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摘要
浩布高铅锌铜锡矿床是以铅锌铜锡为主的大型矽卡岩矿床，产于燕山晚期石英二长岩－黑云母花岗岩与下二叠统大石寨组大理岩接触带内。区域重磁资料是圈定岩体、研究铅锌铜锡多金属成矿地质环境的重要依据。在矿体上方呈现高极化率、高磁、低电阻率异常。电法、磁法、化探是寻找该类型矿床的主要方法
The Haobugao deposit is a large-sized skarn one dominated by lead, zinc, copper and tin,which occurs in the contact between the late Yanshannian quartz monzonite-granite and marble of Dashizhai Formation of Lower Permian. Regional gravity and magnetic information can provide the important basis for outlining rock bodies and studying metallogenic background of the polymetallic deposit.High polarizability,high magnetics and low resistivity are displayed above the ore bodies. Electrical method, magnetic survey and geochemical exploration are principal methods for prospecting of the similar deposits
The Haobugao deposit is a large-sized skarn one dominated by lead, zinc, copper and tin,which occurs in the contact between the late Yanshannian quartz monzonite-granite and marble of Dashizhai Formation of Lower Permian. Regional gravity and magnetic information can provide the important basis for outlining rock bodies and studying metallogenic background of the polymetallic deposit.High polarizability,high magnetics and low resistivity are displayed above the ore bodies. Electrical method, magnetic survey and geochemical exploration are principal methods for prospecting of the similar deposits
引文
1张德全．浩布高铅锌铜锡矽卡岩矿床分带及成因探讨．大兴安岭及邻区铜多金属矿床论文集．北京：地震出版社，19932A．г．塔尔霍夫等．地球物理方法的综合应用．北京：地质出版社，1988
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