Tungsten Enrichment in the South China-type Massive Sulphide Deposits

被引：4

作者：

顾连兴

杨浩

郑素娟

廖静娟

机构：

[1] DepartmentofEarthSciencesNanjingUniversity,Nanjing,,DepartmentofEarthSciences,NanjingUniversity,Nanjing,,DepartmentofEarthSciences,NanjingUniversity,Nanjing,,DepartmentofEarthSciences,NanjingUniversity,Nanjing,,

来源：

Chinese Journal of Geochemistry(English Language Edition) | 1992年 / 04期

关键词：

Zhang; Tungsten Enrichment in the South China-type Massive Sulphide Deposits; type;

D O I：

暂无

中图分类号：

学科分类号：

摘要：

<正> Tungsten is a characteristic element of the South China-type massive sulphide deposits that wereformed on the continental crust.The high contents of tungsten in these deposits are attributed to the pri-mary enrichment of this element in the basement sequences of the region,providing an indication of thetungsten-enrichment in the continental crust.Tungsten in the basement sequences was mobilized and trans-ported to the massive sulphides by a combination of different geological processes such as terrigenoussedimentation,submarine hydrothermal deposition and magmatic hydrothermal superimposition.

引用

页码：344 / 351

页数：8