Implications of 770 Ma Rhyolitic Tuffs, eastern South China Craton in constraining the tectonic setting of the Nanhua Basin

Liang Qi, Yajun Xu, Peter A. Cawood, Wei Wang, Yuansheng Du

Research output: Contribution to journalArticleResearchpeer-review

Abstract

Mid-Neoproterozoic magmatic rocks from the southeastern part of the Nanhua Basin constrain the tectonic setting of the basin. Data from rhyolitic tuffs of the Louqian Formation that overlie the Cathaysia Block in southeastern South China indicate accumulation of the unit at ca. 770 Ma, and provide an upper age limit on collisional assembly of the Yangtze and Cathaysia blocks. The zircons within the tuffs display largely positive ε Hf (t) (−3.66 to +13.94) and juvenile T DM (Hf) values (1.74–0.90 Ga), which indicate involvement of Neoproterozoic to late Paleoproterozoic crustal materials in their generation. Geochemically, the tuffs are peraluminous and characterized by both A-type and arc affinities with high SiO 2 , Ga, accentuated negative Eu anomalies, strong depletion in high field strength elements and high zircon saturation temperatures (T Zr ), which are comparable to contemporaneous (800–750 Ma) felsic rocks from the northwestern of the Nanhua Basin. These characteristics suggest the Nanhua Basin lay inboard of a convergent plate margin arc. This arc is represented by 860–730 Ma magmatism along the western and northern margin of the South China Craton (Panxi-Hannan Belt), with the Nanhua Basin occupying an upper plate, back arc setting.

Original languageEnglish
Pages (from-to)842-858
Number of pages17
JournalLithos
Volume324-325
DOIs
Publication statusPublished - 1 Jan 2019

Keywords

  • Back-arc setting
  • Louqian formation
  • Mid-Neoproterozoic
  • Nanhua basin
  • Rhyolite tuff

Cite this

@article{5750c7e7c9a24dc4aa845f4524915ab2,
title = "Implications of 770 Ma Rhyolitic Tuffs, eastern South China Craton in constraining the tectonic setting of the Nanhua Basin",
abstract = "Mid-Neoproterozoic magmatic rocks from the southeastern part of the Nanhua Basin constrain the tectonic setting of the basin. Data from rhyolitic tuffs of the Louqian Formation that overlie the Cathaysia Block in southeastern South China indicate accumulation of the unit at ca. 770 Ma, and provide an upper age limit on collisional assembly of the Yangtze and Cathaysia blocks. The zircons within the tuffs display largely positive ε Hf (t) (−3.66 to +13.94) and juvenile T DM (Hf) values (1.74–0.90 Ga), which indicate involvement of Neoproterozoic to late Paleoproterozoic crustal materials in their generation. Geochemically, the tuffs are peraluminous and characterized by both A-type and arc affinities with high SiO 2 , Ga, accentuated negative Eu anomalies, strong depletion in high field strength elements and high zircon saturation temperatures (T Zr ), which are comparable to contemporaneous (800–750 Ma) felsic rocks from the northwestern of the Nanhua Basin. These characteristics suggest the Nanhua Basin lay inboard of a convergent plate margin arc. This arc is represented by 860–730 Ma magmatism along the western and northern margin of the South China Craton (Panxi-Hannan Belt), with the Nanhua Basin occupying an upper plate, back arc setting.",
keywords = "Back-arc setting, Louqian formation, Mid-Neoproterozoic, Nanhua basin, Rhyolite tuff",
author = "Liang Qi and Yajun Xu and Cawood, {Peter A.} and Wei Wang and Yuansheng Du",
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doi = "10.1016/j.lithos.2018.12.004",
language = "English",
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Implications of 770 Ma Rhyolitic Tuffs, eastern South China Craton in constraining the tectonic setting of the Nanhua Basin. / Qi, Liang; Xu, Yajun; Cawood, Peter A.; Wang, Wei; Du, Yuansheng.

In: Lithos, Vol. 324-325, 01.01.2019, p. 842-858.

Research output: Contribution to journalArticleResearchpeer-review

TY - JOUR

T1 - Implications of 770 Ma Rhyolitic Tuffs, eastern South China Craton in constraining the tectonic setting of the Nanhua Basin

AU - Qi, Liang

AU - Xu, Yajun

AU - Cawood, Peter A.

AU - Wang, Wei

AU - Du, Yuansheng

PY - 2019/1/1

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N2 - Mid-Neoproterozoic magmatic rocks from the southeastern part of the Nanhua Basin constrain the tectonic setting of the basin. Data from rhyolitic tuffs of the Louqian Formation that overlie the Cathaysia Block in southeastern South China indicate accumulation of the unit at ca. 770 Ma, and provide an upper age limit on collisional assembly of the Yangtze and Cathaysia blocks. The zircons within the tuffs display largely positive ε Hf (t) (−3.66 to +13.94) and juvenile T DM (Hf) values (1.74–0.90 Ga), which indicate involvement of Neoproterozoic to late Paleoproterozoic crustal materials in their generation. Geochemically, the tuffs are peraluminous and characterized by both A-type and arc affinities with high SiO 2 , Ga, accentuated negative Eu anomalies, strong depletion in high field strength elements and high zircon saturation temperatures (T Zr ), which are comparable to contemporaneous (800–750 Ma) felsic rocks from the northwestern of the Nanhua Basin. These characteristics suggest the Nanhua Basin lay inboard of a convergent plate margin arc. This arc is represented by 860–730 Ma magmatism along the western and northern margin of the South China Craton (Panxi-Hannan Belt), with the Nanhua Basin occupying an upper plate, back arc setting.

AB - Mid-Neoproterozoic magmatic rocks from the southeastern part of the Nanhua Basin constrain the tectonic setting of the basin. Data from rhyolitic tuffs of the Louqian Formation that overlie the Cathaysia Block in southeastern South China indicate accumulation of the unit at ca. 770 Ma, and provide an upper age limit on collisional assembly of the Yangtze and Cathaysia blocks. The zircons within the tuffs display largely positive ε Hf (t) (−3.66 to +13.94) and juvenile T DM (Hf) values (1.74–0.90 Ga), which indicate involvement of Neoproterozoic to late Paleoproterozoic crustal materials in their generation. Geochemically, the tuffs are peraluminous and characterized by both A-type and arc affinities with high SiO 2 , Ga, accentuated negative Eu anomalies, strong depletion in high field strength elements and high zircon saturation temperatures (T Zr ), which are comparable to contemporaneous (800–750 Ma) felsic rocks from the northwestern of the Nanhua Basin. These characteristics suggest the Nanhua Basin lay inboard of a convergent plate margin arc. This arc is represented by 860–730 Ma magmatism along the western and northern margin of the South China Craton (Panxi-Hannan Belt), with the Nanhua Basin occupying an upper plate, back arc setting.

KW - Back-arc setting

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KW - Mid-Neoproterozoic

KW - Nanhua basin

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