火山沉积矿床

硫同位素组成δ34S为7.00‰～23.00‰，黄铁矿是含矿热液以堆积、充填和交代方式形成，黄铁矿床为火山热水沉积矿床。

Sulfur isotopic composition is 7.00 ‰~ 0.90 ‰ . The pyrite mineral had genetic tie with concentration , filling and metasomatism of the ore bearing hydrothermal solution , and the deposits represent a sedimentary deposit caused by volcanic hydrothermal solution .

滇东南喷流沉积块状硫化物特征与矿床成因华南海相火山喷流沉积矿床成因研究简评&兼述徐克勤教授在该领域的重大贡献

CHARACTERISTICS AND GENESIS OF EXHALATIVE SEDIMENTARY MASSIVE SULFIDES IN SOUTHEASTERN YUNNAN PROVINCE A Brief Review for the Study on Genesis of the Submarine Volcanic Exhalative Sedimentary Deposits in South China

宁芜向山地区火山热水沉积黄铁矿矿床地质概念模型

Theoretical model for hot-water sedimentary pyrite deposits , Xiangshan district , nanjing Wuhu region

该矿床可分为火山气液沉积铜矿床和斑岩型铜矿床两种类型。

The copper deposits may be grouped into two types : the volcanic exhalative sedimentary copper deposit and porphyry copper deposit .