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Multi-Order and Multi-Center Metallogenic Zoning of Yinshan Cu-Au Polymetallic Ore Deposit,Jiangxi Province,China
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作者 Mo Cehui Liu Danying Feng Zhiwen Xia WeflwaChina University of Geosciences , Wuhan 430074 《Journal of Earth Science》 SCIE CAS CSCD 1993年第1期70-73,共4页
Yinshan anticline is the product of tectono-dynamic deformation-metamorphism.Along the axis ofthe anticline exists a brittle-ductile shearing zone which obviously controls the ore-formation.Mineralization occurs along... Yinshan anticline is the product of tectono-dynamic deformation-metamorphism.Along the axis ofthe anticline exists a brittle-ductile shearing zone which obviously controls the ore-formation.Mineralization occurs along the axis of the anticline in a width of about 1000m.In the mining area,volca-no-subvolcanic rocks of Early Yanshan period are divided into three cycles:I intermediate acidic dacite lavaand dacite porphyry;Ⅱacidic amphibole liparite and quartz porphyry;Ⅲ intermediate andesite porphyrite.Among them activities ofⅠand Ⅱ cycles are more intensive and are intimately related to the mineralization.Yinshan ore deposit is the result of combinative processes of tectono-dynamic and volcano—magmatic hydrothermal fluids,so that there are two centers of metallogenic zoning,one being the axialstrain zone of Yinshan anticline which is the center of first order,and the other being porphyry stock,2ndorder. 展开更多
关键词 yinshan polymetallic deposit multi-order and multi-center metallogenic zoning brittle-ductile shearing zone porphyry stock .
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