Petrogenesis of early Jurassic basalts in southern Jiangxi Province, South China: Implications for the thermal state of the Mesozoic mantle beneath South China

Early Jurassic bimodal volcanic and intrusive rocks in southern South China show distinct associations and distribution patterns in comparison with those of the Middle Jurassic and Cretaceous rocks in the area. It is widely accepted that these rocks formed in an extensional setting, although the tim...

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Main Authors: Cen, T., Li, W., Wang, Xuan-Ce, Pang, C., Li, Zheng-Xiang, Xing, G., Zhao, X., Tao, J.
Format: Journal Article
Published: Elsevier BV 2016
Online Access:http://purl.org/au-research/grants/arc/FT140100826
http://hdl.handle.net/20.500.11937/14003
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author Cen, T.
Li, W.
Wang, Xuan-Ce
Pang, C.
Li, Zheng-Xiang
Xing, G.
Zhao, X.
Tao, J.
author_facet Cen, T.
Li, W.
Wang, Xuan-Ce
Pang, C.
Li, Zheng-Xiang
Xing, G.
Zhao, X.
Tao, J.
author_sort Cen, T.
building Curtin Institutional Repository
collection Online Access
description Early Jurassic bimodal volcanic and intrusive rocks in southern South China show distinct associations and distribution patterns in comparison with those of the Middle Jurassic and Cretaceous rocks in the area. It is widely accepted that these rocks formed in an extensional setting, although the timing of the onset and the tectonic driver for extension are debated. Here, we present systematic LA–ICP–MS zircon U–Pb ages, whole-rock geochemistry and Sr–Nd isotope data for bimodal volcanic rocks from the Changpu Formation in the Changpu–Baimianshi and Dongkeng–Linjiang basins in southern Jiangxi Province, South China. Zircon U–Pb ages indicate that the bimodal volcanic rocks erupted at ca. 190 Ma, contemporaneous with the Fankeng basalts (~ 183 Ma). A compilation of geochronological results demonstrates that basin-scale basaltic eruptions occurred during the Early Jurassic within a relatively short interval (< 5 Ma). These Early Jurassic basalts have tholeiitic compositions and OIB-like trace element distribution patterns.Geochemical analyses show that the basalts were derived from depleted asthenospheric mantle, dominated by a volatile-free peridotite source. The calculated primary melt compositions suggest that the basalts formed at 1.9–2.1 GPa, with melting temperatures of 1378 °C–1405 °C and a mantle potential temperature (TP) ranging from 1383 °C to 1407 °C. The temperature range is somewhat hotter than normal mid-ocean-basalt (MORB) mantle but similar to an intra-plate continental mantle setting, such as the Basin and Range Province in western North America. This study provides an important constraint on the Early Jurassic mantle thermal state beneath South China.
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spelling curtin-20.500.11937-140032023-01-25T06:57:12Z Petrogenesis of early Jurassic basalts in southern Jiangxi Province, South China: Implications for the thermal state of the Mesozoic mantle beneath South China Cen, T. Li, W. Wang, Xuan-Ce Pang, C. Li, Zheng-Xiang Xing, G. Zhao, X. Tao, J. Early Jurassic bimodal volcanic and intrusive rocks in southern South China show distinct associations and distribution patterns in comparison with those of the Middle Jurassic and Cretaceous rocks in the area. It is widely accepted that these rocks formed in an extensional setting, although the timing of the onset and the tectonic driver for extension are debated. Here, we present systematic LA–ICP–MS zircon U–Pb ages, whole-rock geochemistry and Sr–Nd isotope data for bimodal volcanic rocks from the Changpu Formation in the Changpu–Baimianshi and Dongkeng–Linjiang basins in southern Jiangxi Province, South China. Zircon U–Pb ages indicate that the bimodal volcanic rocks erupted at ca. 190 Ma, contemporaneous with the Fankeng basalts (~ 183 Ma). A compilation of geochronological results demonstrates that basin-scale basaltic eruptions occurred during the Early Jurassic within a relatively short interval (< 5 Ma). These Early Jurassic basalts have tholeiitic compositions and OIB-like trace element distribution patterns.Geochemical analyses show that the basalts were derived from depleted asthenospheric mantle, dominated by a volatile-free peridotite source. The calculated primary melt compositions suggest that the basalts formed at 1.9–2.1 GPa, with melting temperatures of 1378 °C–1405 °C and a mantle potential temperature (TP) ranging from 1383 °C to 1407 °C. The temperature range is somewhat hotter than normal mid-ocean-basalt (MORB) mantle but similar to an intra-plate continental mantle setting, such as the Basin and Range Province in western North America. This study provides an important constraint on the Early Jurassic mantle thermal state beneath South China. 2016 Journal Article http://hdl.handle.net/20.500.11937/14003 10.1016/j.lithos.2016.03.022 http://purl.org/au-research/grants/arc/FT140100826 http://purl.org/au-research/grants/arc/FL150100133 Elsevier BV restricted
spellingShingle Cen, T.
Li, W.
Wang, Xuan-Ce
Pang, C.
Li, Zheng-Xiang
Xing, G.
Zhao, X.
Tao, J.
Petrogenesis of early Jurassic basalts in southern Jiangxi Province, South China: Implications for the thermal state of the Mesozoic mantle beneath South China
title Petrogenesis of early Jurassic basalts in southern Jiangxi Province, South China: Implications for the thermal state of the Mesozoic mantle beneath South China
title_full Petrogenesis of early Jurassic basalts in southern Jiangxi Province, South China: Implications for the thermal state of the Mesozoic mantle beneath South China
title_fullStr Petrogenesis of early Jurassic basalts in southern Jiangxi Province, South China: Implications for the thermal state of the Mesozoic mantle beneath South China
title_full_unstemmed Petrogenesis of early Jurassic basalts in southern Jiangxi Province, South China: Implications for the thermal state of the Mesozoic mantle beneath South China
title_short Petrogenesis of early Jurassic basalts in southern Jiangxi Province, South China: Implications for the thermal state of the Mesozoic mantle beneath South China
title_sort petrogenesis of early jurassic basalts in southern jiangxi province, south china: implications for the thermal state of the mesozoic mantle beneath south china
url http://purl.org/au-research/grants/arc/FT140100826
http://purl.org/au-research/grants/arc/FT140100826
http://hdl.handle.net/20.500.11937/14003