|Table of Contents|

Tectonic Transformation of Proto- and Paleo-Tethys and the Metallization of Magmatic Ni-Cu-Co Sufide Deposits in Kunlun Orogen, Northwest China(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2022年第01期
Page:
1-19
Research Field:
基础地质与矿床地质
Publishing date:

Info

Title:
Tectonic Transformation of Proto- and Paleo-Tethys and the Metallization of Magmatic Ni-Cu-Co Sufide Deposits in Kunlun Orogen, Northwest China
Author(s):
LI Wen-yuan1; 2; 3;  ZHANG Zhao-wei1; 2;  WANG Ya-lei1; 2; 4;  ZHANG Jiang-wei1; 2;  YOU Min-xin1; 2; 4;  ZHANG Zhi-bing5;  Namkha NORBU6
(1. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits of Ministry of Natural Resources, Xi'an 710054, Shaanxi, China; 2. Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, Shaanxi, China; 3. China-SCO Geosciences Research Center, Xi'an 710054, Shaanxi, China; 4. Graduate School of Chinese Academy of Geological Sciences, Beijing 100037, China; 5. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 6. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China)
Keywords:
magmatic Cu-Ni-Co sulfide deposit;  mafic-ultramafic rock;  Proto-Tethy;  Paleo-Tethy;  tectonic transformation;  metallization;  East Kunlun
PACS:
P611
DOI:
10.19814/j.jese.2021.08033
Abstract:
The research of Tethys tectonic domain shows more and more characteristics of Proto-Tethys, Paleo-Tethys and Neo-Tethys, among which the research of formation and evolution of Paleo-Tethys ocean and its mineralization are relatively weak, particularly when Paleo-Tethys began cracking almostly lackes necessary research. On the basis of the discovery of Xiarihamu super-large Cu-Ni-Co sulfide deposit at the end of Early Paleozoic in East Kunlun, and the characteristics of a number of magmatic Cu-Ni-Co sulfide deposits dating between the end of Early Paleozoic and early Late Paleozoic in East Kunlun, Southern Qilian and Alkin, it is proposed that they represent the results of Paleo-Tethys cracking. It is believed that after the collision closure for Proto-Tethys ocean in the same period as Paleo-Asian ocean at the end of Silurian, and as a result of mantle plume, the modified asthenosphere is partially melted and the northern margin of Gondwana continent is cracked, which results in the formation of Xiarihamu deposit related to the mantle-derived mafic-ultramafic rock. Turn of Early and Late Paleozoic is the beginning of Paleo-Tethys ocean cracking, and at this time, Qinling-Qilian-Kunlun ocean as the representative of Proto-Tethys ocean has been closed. Although Paleo-Asian ocean as a back-arc basin of Proto-Tethys is not yet closed, Xiarihamu deposit is the product of the re-cracking of continental crust after Proto-Tethys orogeny, and is not formed in the environment of Proto-Tethys island arc or post-collision. Mineralalogy and geochemical results show that although the arc magma information with depletion of Nb, Ta, Ti in Xiarihamu deposit, it is significantly different from Alaska rock body in the island arc environment; Xiarihamu deposit has more pyroxenite, less magnetite content, and primary magma with high-Al2O3, etc. According to the existing mineralization, combined with the research of closed ophiolites and shell subduction returning eclogite of Proto-Tethys ocean, and the characteristics of the regional unconformity of Early Devonian formation and the distribution of bimodal volcanic rocks contemporary with the magmatic Cu-Ni-Co sulfide deposits in East Kunlun, the Early Devonian magmatic Cu-Ni-Co sulfide deposit represented by Xiarihamu deposit is not only the first super-large magmatic Ni-Co sulfide deposit discovered in the global Tethys metallogenic domain, but also represents the new magmatic Cu-Ni-Co important ore-forming event, which is the product of the major geological event of Paleo-Tethys cracking. Strengthening the research of deep magmatic sources and ore-forming processes of mineralized and not syn-exhumation mafic-ultramafic rocks in the orogenic belts, will help revealing the geodynamics mechanisms and processes of the initial tectonic evolution of Paleo-Tethys ocean.

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Last Update: 2022-02-25