The Dynamic Sulfide Saturation Process and a Possible Slab Break-off Model for the Giant Xiarihamu Magmatic Nickel Ore Deposit in the East Kunlun Orogenic Belt, Northern Qinghai-Tibet Plateau, China-Reference-Cited by-同舟云学术

The Dynamic Sulfide Saturation Process and a Possible Slab Break-off Model for the Giant Xiarihamu Magmatic Nickel Ore Deposit in the East Kunlun Orogenic Belt, Northern Qinghai-Tibet Plateau, China

Published:2018-09-01 Issue:6 Volume:113 Page:1383-1417
ISSN:1554-0774
Container-title:Economic Geology
language:en
Short-container-title:

Author:

Liu YueGao¹,Li WenYuan¹,Jia QunZi¹,Zhang ZhaoWei¹,Wang ZhiAn²,Zhang ZhiBing³,Zhang JiangWei¹,Qian Bing¹

Affiliation:

1. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Ministry of Land and Resources, Xi’an Center of China Geological Survey, Xi’an 710054, P.R. China

2. No. 5 Geological and Mineral Survey Institute, Qinghai Bureau of Geology and Mineral Resources, Xining 810000, P.R. China

3. Institute of Mineral Resources Research, China Metallurgical Geology Bureau, Beijing 100025, P.R. China

Publisher

Society of Economic Geologists

Subject

Economic Geology,Geochemistry and Petrology,Geology,Geophysics

Link

https://pubs.geoscienceworld.org/segweb/economicgeology/article-pdf/113/6/1383/4530415/1383-1417.pdf

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