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辽西大红石砬子金矿床地质特征及找矿标志

Geological characteristics and prospecting indicator of Dahongshilazi Gold Deposit in western Liaoning

  • 摘要: 大红石砬子金矿床为辽西地区新发现的隐爆角砾岩型金矿床。运用地、物、化综合勘查方法,结合探矿工程,发现了隐爆角砾岩体,即矿化蚀变带,并圈定了4条矿体。矿体受北东向断裂和环形断裂控制,均赋存在中侏罗统髫髻山组安山岩与下白垩统义县组流纹岩接触带的隐爆角砾岩体中。下白垩统义县组地层、隐爆角砾岩、北东向断裂与环状断裂和流纹斑岩脉,以及黄铁矿化、硅化、碳酸盐化等围岩蚀变为主要的地质找矿标志;Au-Ag-As-Pb-Zn-Cu-Sb-Mo土壤综合异常是地球化学找矿标志;低阻高极化特征为重要的地球物理找矿标志。4条矿体在走向和倾向上均未封闭,具有进一步找矿的潜力,通过开展综合地质找矿,矿床规模有望达到大中型。

     

    Abstract: The Dahongshilazi Gold Deposit is a newly discovered cryptoexplosive breccia type deposit in western Liaoning.Based on the comprehensive exploration method combining geological,geophysical and geochemical prospecting as well as exploration projects,the cryptoexplosive breccia body that is mineralization alteration zone is discovered and 4 ore bodies are delineated.The ore bodies are controlled by NE fault and ringed fault and hosted in the cryptoexplosive breccia on the contact zone of middle Jurassic Tiaojishan Formation andesite and lower cretaceous Yixian Formation rhyolite.The lower cretaceous Yixian Formation strata,cryptoexplosive breccia,NE fault and ringed fault,rhyolite porphyry,and such wall rock alteration as pyritization,silicification,and carbonatization are major prospecting indicators.Au-Ag-As-Pb-Zn-Cu-Sb-Mo comprehensive soil anomaly is the geochemical indicator; the characteristic of low resistance and high polarization is an important geophysical indicator.Four ore bodies are not sealed in strike or dip and bear potential for further prospecting.Via comprehensive geological prospecting,the deposit scale is expected to reach medium to large scale.

     

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