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.
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)
关键词
同沉积断裂
热水溶液
裂陷裂谷盆地
克拉通盆地
synsedimentary fault
thermal fluid
chasmic and rift basin
cratonic basin
