Source of ore-forming material and metallogenic age of the Zheboshan gold deposit, western Sichuan Province, China

被引:1
|
作者
Ji, HB [1 ]
Li, CY
Wen, JM
机构
[1] Chinese Acad Sci, Open Lab Ore Deposit Geochem, Guiyang 55000, Peoples R China
[2] Sichuan Bur Geol & Mineral Resources, NW Sichuan Geol Party, Mianyang 621000, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 1998年 / 43卷 / 08期
关键词
ICP-MS; element; Rb-Sr isotopes; ore-forming material; metallogenic age;
D O I
10.1007/BF02883578
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The Zheboshan gold deposit, which is located in the "Gold Triangle" area on the borders of Sichuan, Gansu and Shaanxi provinces, is a very complicated micro-fine disseminated gold deposit. Considering the ICP-MS measurements and Rb and Sr isotope data, it is suggested that the ore-forming materials may have come from the quartz-amphibole porphyrite dykes. It is also suggested that the age of ore deposit is generally consistent with the age of formation of the quartz-amphibole porphyrite. It is further deduced that the deposit is a magmatic hydrothermal ore deposit.
引用
收藏
页码:684 / 690
页数:7
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