扬子北缘及南秦岭铅锌重晶石锰钒矿成矿地质背景  

METALLOGENIC GEOLOGY OF LEAD-ZINC-BARITE-MANGANESE-VANADIUM MINERALIZATION IN THE NORTH MARGIN OF THE YANGTZE PLATE AND SOUTH QINLING MOUNTAINS

作　　者：倪新远 陈高潮 彭俊英 王炬川 张俊良 张清盛 孔文年 

机构地区：[1]新疆第二区域地质调查大队,新疆昌吉831100 [2]陕西省地质调查院,西安710016

出　　处：《陕西地质》2010年第1期34-38,共5页Geology of Shaanxi

基　　金：中国地质调查局<1:25万南江市幅(I48C004004);安康市幅(I49C004001)区域地质调查(修测)>项目(编号:1212010510406)

摘　　要：扬子北缘铅锌矿、锰矿、重晶石、毒重石矿和黑色岩系钒矿成矿地质条件具有一定规律性,属于受沉积盆地控制统一成矿系列,形成于扬子地块北部边缘裂解环境次级盆地中,成矿受所处构造位置、沉积盆地、同生断裂、沉积相控制。Metallogenic geology of lead-zinc, manganese, barite, witherite and black shalehosted vanadium ores occurring in the north margin of the Yangtze plate is an attribute of occurrences in sedimentary basins, mainly forming in secondary basins at the north margin of the Yangtze Plate. The lead-zinc, manganese, barite, witherite and black shale-hosted vanadium mineralization is confined to the tectonic position, sedimentary basin, syngenetic fault and sedimentary facies.

关 键 词：同沉积断裂 热水溶液 裂陷裂谷盆地 克拉通盆地 

分 类 号：P618.41[天文地球—矿床学]