摘要
概述了湖北黄石铅锌矿田的地质、微量元素、稳定同位素和矿物包裹体等特征,提出了该矿田的矿床为同生沉积—热卤水改造成因及找矿方向。
Characteristica of the geology,trace elemients,stable isotopes and mineral inclusions of the Huangshi Pb-Zn ore field inHubei Provinoe are summarized.The author holds that the ore field is of hypergenic syngenetic sedimentary-hot brine reformationorigin.In this paper the guide for ore exploration is given.
出处
《地质与勘探》
CAS
CSCD
北大核心
1993年第4期52-56,共5页
Geology and Exploration