Plate subduction, oxygen fugacity, and mineralization

He LIU; Renqiang LIAO; Lipeng ZHANG; Congying LI; Weidong SUN

doi:10.1007/s00343-019-8339-y

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Plate subduction, oxygen fugacity, and mineralization

Geology | Updated：2023-04-27

- Plate subduction, oxygen fugacity, and mineralization
- Journal of Oceanology and Limnology Vol. 38, Issue 1, Pages: 64-74(2020)
- Affiliations：
  
  1.Key Laboratory of Marine Geology and Environment, Center of Deep-Sea Research, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
  2.Laboratory for Marine Mineral Resources, Laboratory for Marine Biology and Biotechnology, Pilot National Laboratory for Marine Science and Technology, Qingdao 266071, China
  3.Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
  4.University of Chinese Academy of Sciences, Beijing 100049, China
- Author bio：
  
  SUN Weidong, weidongsun@qdio.ac.cn
- Funds：
- DOI：10.1007/s00343-019-8339-y
  CLC：
- Received：27 November 2018，
  
  Accepted：18 January 2019，
  
  Online First：11 April 2019，
  
  Published：2020-01
- Accepted：
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He LIU, Renqiang LIAO, Lipeng ZHANG, et al. Plate subduction, oxygen fugacity, and mineralization[J]. Journal of Oceanology and Limnology, 2020, 38(1): 64-74.
DOI：

He LIU, Renqiang LIAO, Lipeng ZHANG, et al. Plate subduction, oxygen fugacity, and mineralization[J]. Journal of Oceanology and Limnology, 2020, 38(1): 64-74. DOI： 10.1007/s00343-019-8339-y.

摘要

Abstract

Plate subduction is the largest natural factory that processes elements

which controls recycling and mineralization of a variety of elements. There are three major ore deposit belts in the world:the circumPacific

the central Asian

and the Tethys belts. All the three belts are closely associated with plate subductions

the mechanism remains obscure. We approached this problem from systematic studies on the behaviours of elements during geologic processes. This contribution summaries the recent progress of our research group. Our results suggest that porphyry Cu deposits form through partial melting of subducted young oceanic crust under oxygen fugacities higher than ·FMQ~+1.5

which is promoted after the elevation of atmospheric oxygen at ca. 550 Ma. Tin deposits are associated with reducing magmatic rocks formed as a consequence of slab rollback. The Neo-Tethys tectonic regime hosts more than 60% of the world's total Sn reserves. This is due to the reducing environment formed during the subduction of organic rich sediments. For the same reason

porphyry Cu deposits formed in the late stages during the closure of the Neo-Tethys Ocean. Tungsten deposits are also controlled by slab rollback

but is not so sensitive to oxygen fugacity. Subduction related W/Sn deposits are mostly accompanied by abundant accessory fluorites due to the breakdown of phengite and apatite. Decomposition of phengite is also significant for hard rock lithium deposits

whereas orogenic belt resulted from plate subduction promote the formation of Li brine deposits. Cretaceous red bed basins near the Nanling region are favorable for Li brines. Both Mo and Re are enriched in the oxidationreduction cycle during surface processes

and may get further enriched once Mo-

Re-enriched sediments are subducted and involved in magmatism. During plate subduction

Mo and Re fractionate from each other. Molybdenum is mainly hosted in porphyry Mo deposits and to a less extent

porphyry Cu-Mo deposits

whereas Re is predominantly hosted in porphyry Cu-Mo deposits and sedimentary sulfide deposits.

关键词

Keywords

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