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机构地区:[1]成都理工大学地球科学学院,四川成都610059
出 处:《四川有色金属》2014年第4期48-52,共5页Sichuan Nonferrous Metals
基 金:成都理工大学地球科学学院资源勘查工程系(固体矿产)资源勘查工程专业教育部卓越工程师教育培养计划项目;编号:13z002-07;"卓越计划"背景下资源勘查工程专业实践教学体系的建设与改革;编号:13JGZ16
摘 要:稻城县竹鸡顶铜矿位处松潘甘孜印支地槽褶皱系义敦岛弧带南段金沙江超壳型深大断裂带东侧的得荣褶皱带和乡城褶皱带,属川滇“三江”成矿带重要组成之一.出露古生界寒武系~二叠系、中生界三叠系和新生界地层.矿石矿物以黄铜矿为主,少量斑铜矿、孔雀石和兰铜矿,其他金属矿物有黄铁矿、褐铁矿、方铅矿、磁铁矿、磁黄铁矿等.矿石主要结构为:微~细粒结构.浸染状、脉状、网脉状构造为主,块状构造少量.矿体主要产于褶皱带断裂破碎带中.找矿标志为地表岩石发生的岩石次生变化,地球物理地球化学特征异常以及遥感影像中出现的色异常和环形构造.Daocheng county bamboo chicken top copper fold system YiDui island arc zone southern Yangtze river mine located in songpan ganzi indosinian geosynclinal super shell type deep fault zone on the east side of the rong fold belt and rural-urban fold belt,which belongs to sichuan and yunnan “sanjiang” metallogenic belt is an important one.Exposed upper Paleozoic Cambrian - yanchang formation of Permian, Mesozoic and Cenozoic strata.Give priority to with chalcopyrite ore mineral, a small amount of spot copper, copper ore, malachite and other metal minerals are pyrite, limonite, galena, magnetite, magnetic pyrite and so on. Ore main structure is: the micro - fine grained structure.Disseminated, vein and vein structure is given priority to, block structure a little. Ore body is mainly produced in fold belt in the fractured zone. Ore-prospecting criteria for the rock secondary changes of the surface rock, geophysical geochemical anomaly and remote sensing image in color abnormal and ring structures.
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