Discovery of the Archean Magmatic Cu-Ni Sulfide Deposit in China——Taoke Deposit, Shandong Province

被引：0
|
作者：
SUN Tao [1 ]
WANG Denghong [2 ]
LI Chao [3 ]
ZHANG Zengqi [4 ]
SUN Bin [4 ]
CHENG Wei [4 ]
LI Wanting [1 ]
ZHANG Aiping [1 ]
机构：
[1] School of Earth Sciences, Yunnan University, MNR Key Laboratory of Sanjiang Metallogeny and Resources Exploration and Utilization
[2] MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences
[3] National Research Center for Geoanalysis, Key Laboratory of Re-Os Isotope Geochemistry,CAGS
[4] Shandong Institute of Geological Sciences
来源：
Acta Geologica Sinica(English Edition) | 2020年 / 02期
基金：
美国国家科学基金会;
关键词：
Discovery of the Archean Magmatic Cu-Ni Sulfide Deposit in China; Shandong Province; Taoke Deposit;
D O I：
暂无
中图分类号：
P618.41 [铜]; P618.63 [镍];
学科分类号：
0709 ; 081803 ;
摘要：
Objective The formation ages of global magmatic sulfide Ni-Cu deposits are from Archean to Mesozoic, the Neoarchean and Neoproterozoic are the two peaks. In China, the formation ages of magmatic sulfide deposits are from Proterozoic to Mesozoic, and the Neoproterozoic and late Paleozoic are the two peaks,. Compared with the global
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页码：561 / 562
页数：2
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