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Three late-Mesozoic fluorite deposit belts in southeast China and links to subduction of the (paleo-) Pacific plate
Yan, Haibo1,2,3; Ding, Xing1,3; Ling, Mingxing1; Li, Congying4,5; Harlov, Daniel E.6,7,8; Sun, Weidong4,5
2021-02-01
发表期刊ORE GEOLOGY REVIEWS
ISSN0169-1368
卷号129页码:11
通讯作者Ding, Xing([email protected]) ; Sun, Weidong([email protected])
摘要Rocks and ore deposits in subduction zones can provide clues to material cycling and related subduction processes. Here we demonstrate, based upon a new data compilation from more than 240 late-Mesozoic fluorite deposits in southeast China that most of them can be divided into three fluorite deposit belts (FDB) with distinct ages and orientations. The two older inland FDB with a NE-SW orientation were formed at 165-150 Ma and 150-130 Ma, respectively, whereas the younger coastal FDB, roughly perpendicular to the others, was generated at 110-70 Ma. The temporal-spatial distributions of the FDB are compatible with the subduction of the (paleo-) Pacific plate. We propose that the genesis of the earlier two inland FDB was due to northeastward slab rollback during low-angle subduction, while formation of the coastal FDB resulted mainly from high-angle northwestward hot/warm subduction. Large amounts of F, mainly derived from the decomposition of phengite (+/- apatite) in the subducted slabs, could be transported into the overlying crust via F-rich fluids and alkalic magmas. Subsequently, extensive crustal magmatism and fluid activities associated with subduction further concentrate F from the magmas and/or wall-rocks and facilitate fluorite mineralization. This study provides new insights into the interaction between the subducting (paleo-) Pacific plate and overlying eastern Eurasian continent in the late Mesozoic. It also highlights the potential genetic association of F transport/deposition with plate subduction that could be a common phenomenon in ancient and modern subduction zones.
关键词Fluorite deposit Plate subduction Pacific plate Fluorine Slab rollback
DOI10.1016/j.oregeorev.2020.103865
收录类别SCI
语种英语
资助项目National Key R&D Program of China[2016YFC0600408]; National Key R&D Program of China[2016YFC0600204]; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB42000000]; Guangdong Major Project of Basic and Applied Basic Research[2019B030302013]; Taishan Scholar Program of Shandong[ts201712075]; AoShan Talents Cultivation Program - Qingdao National Laboratory for Marine Science and Technology[2017ASTCP-OS07]
WOS研究方向Geology ; Mineralogy ; Mining & Mineral Processing
WOS类目Geology ; Mineralogy ; Mining & Mineral Processing
WOS记录号WOS:000612803300005
出版者ELSEVIER
引用统计
被引频次:14[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/169698
专题深海极端环境与生命过程研究中心
通讯作者Ding, Xing; Sun, Weidong
作者单位1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
2.Chinese Acad Sci, Guangzhou Inst Geochem, CAS Key Lab Mineral & Metallogeny, Guangzhou 510640, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China
5.Chinese Acad Sci, Inst Oceanog, Ctr Deep Sea Res, Qingdao 266071, Peoples R China
6.Deutches GeoforschungsZent, D-14473 Potsdam, Germany
7.Univ Johannesburg, Dept Geol, POB 524, ZA-2006 Auckland Pk, South Africa
8.China Univ Geosci, Sch Earth Resources, Wuhan 430074, Peoples R China
通讯作者单位中国科学院海洋研究所
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Yan, Haibo,Ding, Xing,Ling, Mingxing,et al. Three late-Mesozoic fluorite deposit belts in southeast China and links to subduction of the (paleo-) Pacific plate[J]. ORE GEOLOGY REVIEWS,2021,129:11.
APA Yan, Haibo,Ding, Xing,Ling, Mingxing,Li, Congying,Harlov, Daniel E.,&Sun, Weidong.(2021).Three late-Mesozoic fluorite deposit belts in southeast China and links to subduction of the (paleo-) Pacific plate.ORE GEOLOGY REVIEWS,129,11.
MLA Yan, Haibo,et al."Three late-Mesozoic fluorite deposit belts in southeast China and links to subduction of the (paleo-) Pacific plate".ORE GEOLOGY REVIEWS 129(2021):11.
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