摘要
在论述秦岭泥盆系层控铅锌矿床的黄铁矿微量元素,硫、铅、氢、氧同位素,矿物气液包裹体均一温度及成分.区域地层元素丰度等方面特征的基础上,提出了该类型属海底含矿热泉溢出沉积和隐伏含矿热泉贯入沉淀的成因模式.
The characteristics of the trace elements in pyrite, the isotopes of S, Pb, O and H, hornogenization temperature and constituents of the fluid inclusions, and the element abundance in the regional strata are given in the article, based on which genetic model is suggested to this type of deposit with deposition of the sea bottom ore-bearing hot spring effluent and deposition of the concealed ore-bearing hot spring injection.
出处
《矿产与地质》
1991年第3期183-190,共8页
Mineral Resources and Geology
关键词
铅锌矿床
成因
模式
泥盆纪
Stratabound lead zinc deposit, Hot spring effluent, Hot spring injection, Genetic model
