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author:

Lin, Musen (Lin, Musen.) [1] (Scholars:林木森) | Peng, Songbai (Peng, Songbai.) [2] | Jiang, Xingfu (Jiang, Xingfu.) [3] | Polat, Ali (Polat, Ali.) [4] | Kusky, Timothy (Kusky, Timothy.) [5] | Wang, Qing (Wang, Qing.) [6] | Deng, Hao (Deng, Hao.) [7]

Indexed by:

Scopus SCIE

Abstract:

The Jiangnan orogenic belt (JOB) has been interpreted as a suture zone between the Yangtze craton and Cathaysian terranes in South China. The Neoproterozoic mafic-ultramafic rocks are extensively exposed in the western JOB, providing an ideal opportunity to study the Neoproterozoic assembly and tectonic evolution of South China. We present integrated field and geochemical studies including LA-ICP-MS zircon U-Pb dating, and whole-rock major and trace element and Sm-Nd isotope analyses of the Neoproterozoic mafic-ultramafic rocks exposed in the northern Guangxi Province, South China. Geochronological results show that the magmatic events took place in two distinct periods: the early Neoproterozoic (861-834 Ma) and the late Neoproterozoic (770-750 Ma). Early Neoproterozoic ultramafic rocks of the Sibao Group have positive epsilon(Nd)(t) values (+ 2.7 to + 6.6) whereas mafic rocks exhibit negative epsilon(Nd)(t) values (-5.8 to -0.9). The basaltic rocks show TiO2 contents of 0.62-0.69 wt.% and Mg-number of 59-65, and also display an enrichment of light rare earth elements (LREEs) and pronounced negative Nb, Ta and Ti anomalies on chondrite- and primitive niantle-normalized diagrams, consistent with subduction-related geochemical signatures. Late Neoproterozoic rocks of the Danzhou Group show epsilon(Nd)(t) values (-123 to +3.19) for both ultramafic and mafic rocks. The basaltic rocks have TiO2 contents of 1.01-1.33 wt.% and Mg-number of 57-60, and have a mixture of MORB- and arc-like geochemical affinities, inferred to have formed in an extensional arc environment. Geochemical signatures suggest that all rock types in this study were derived from subarc mantle wedge sources and underwent various degrees of crustal contamination. Thus, we suggest that subduction may have continued to ca. 750 Ma in the western JOB, implying that the amalgamation event between the Yangtze craton and Cathaysian terranes was later than 750 Ma. (C) 2015 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.

Keyword:

Geochemistry Neoproterozoic mafic-ultramafic rocks Tectonic implications Western Jiangnan orogenic belt Zircon U-Pb dating

Community:

  • [ 1 ] [Lin, Musen]China Univ Geosci, Sch Earth Sci, Wuhan 430074, Peoples R China
  • [ 2 ] [Peng, Songbai]China Univ Geosci, Sch Earth Sci, Wuhan 430074, Peoples R China
  • [ 3 ] [Kusky, Timothy]China Univ Geosci, Sch Earth Sci, Wuhan 430074, Peoples R China
  • [ 4 ] [Deng, Hao]China Univ Geosci, Sch Earth Sci, Wuhan 430074, Peoples R China
  • [ 5 ] [Lin, Musen]Fuzhou Univ, Coll Zijin Min, Fuzhou 350108, Peoples R China
  • [ 6 ] [Peng, Songbai]China Univ Geosci, Ctr Global Tecton, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
  • [ 7 ] [Polat, Ali]China Univ Geosci, Ctr Global Tecton, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
  • [ 8 ] [Kusky, Timothy]China Univ Geosci, Ctr Global Tecton, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
  • [ 9 ] [Deng, Hao]China Univ Geosci, Ctr Global Tecton, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
  • [ 10 ] [Jiang, Xingfu]East China Inst Technol, Coll Earth Sci, Nanchang 330013, Peoples R China
  • [ 11 ] [Polat, Ali]Univ Windsor, Dept Earth & Environm Sci, Windsor, ON N9B 3P4, Canada
  • [ 12 ] [Wang, Qing]China Coal Technol & Engn Grp Corp, Xian Res Inst, Xian 710077, Peoples R China

Reprint 's Address:

  • [Peng, Songbai]China Univ Geosci, Sch Earth Sci, Wuhan 430074, Peoples R China

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Source :

GONDWANA RESEARCH

ISSN: 1342-937X

Year: 2016

Volume: 35

Page: 338-356

6 . 9 5 9

JCR@2016

7 . 2 0 0

JCR@2023

ESI Discipline: GEOSCIENCES;

ESI HC Threshold:196

JCR Journal Grade:1

CAS Journal Grade:1

Cited Count:

WoS CC Cited Count: 45

SCOPUS Cited Count:

ESI Highly Cited Papers on the List: 0 Unfold All

WanFang Cited Count:

Chinese Cited Count:

30 Days PV: 2

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