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The Structural Ore-Controlling Regularity in Hexi Gold Mining Area and its Application in Prospecting

机译:河西金矿区结构矿石控制规律及其在勘探中的应用

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Zhaoye gold zone is located at Lubei Upwarp of North China Platform, south limb of Qixia-Yexian anticlinorium with axis of east-west extending. It is bordered on the east of Yishu large fractured zone. In this area, E—W & NE structures are well developed and formed the fundamental structure pattern of the area. In this area, the major part are covered with Quaternary, the outcropped strata are mainly Archaeozoic Jiaodong Group comprising regional metamorphic rocks of amphibolite facies. The major rock types are amphibolite, biotite leptynite and biotite-plagioclase-horn-blende gneiss and minor amount of schist and marble. The structures are mainly fractures & joints. From west to east, successively occurred Jiaojia fracture, Hexi fracture and Wangershan fracture. They are mainly NE-trending in large scale. Among these fractures, NE & NEE trending metasomatic-anatectic granite are widely outcropped. These are the subsidiary structure in the host rocks of orebody.
机译:Zhaoye Gold Tens位于北瓷平台卢博伊·普通岩,七溪亚思人逆南线南部,拥有东西部延伸的轴。它与沂水大型骨折区以东侧面。在该领域,E-W&NE结构良好地发育并形成了该地区的基本结构模式。在这一领域,主要部分被第四纪覆盖,露头层主要是大型焦思焦东集团,包括倒置倒置的区域变质岩石。主要岩石类型是Amphibolite,Biotite Leptynite和Biotite-Plagioclase-Horn-Blende球茎和少量的分型分泌物和大理石。该结构主要是裂缝和关节。从西到东,连续发生焦家骨折,河西骨折和王氏症骨折。它们主要是大规模的Ne-Trending。在这些裂缝中,NE和NEE趋势态态 - 一种含有偏差花岗岩广泛占外。这些是矿体主体岩石中的子公司结构。

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