Geochronology and Geochemistry of the Late Cretaceous Basalts in the Jiaolai Basin: Constraints on Lithospheric Thinning and Accretion Beneath North China Craton

Previous studies showed a heterogeneous temporal and spatial pattern of lithospheric thinning beneath North China Craton(NCC).The idea is mainly built on the diachronous eruption of the earliest asthenosphere-derived magmas in northern and southern NCC. In this study,we carried out Ar-Ar dating on t...

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Main Authors: Kuang, Y., Pang, Chongjin, Hong, L., Zhong, Y., Xu, Y.
Format: Journal Article
Published: Zhongguo Kexueyuan Guangzhou Diqiu Huaxue Yanjiusuo 2012
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/27676
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author Kuang, Y.
Pang, Chongjin
Hong, L.
Zhong, Y.
Xu, Y.
author_facet Kuang, Y.
Pang, Chongjin
Hong, L.
Zhong, Y.
Xu, Y.
author_sort Kuang, Y.
building Curtin Institutional Repository
collection Online Access
description Previous studies showed a heterogeneous temporal and spatial pattern of lithospheric thinning beneath North China Craton(NCC).The idea is mainly built on the diachronous eruption of the earliest asthenosphere-derived magmas in northern and southern NCC. In this study,we carried out Ar-Ar dating on the Xiguanzhuang tholeiitic basalt(the Jiaolai basin).40 Ar-39 Ar data show that it erupted at 96±3 Ma,thus belonging to the Qingshan Group,earlier than the Daxizhuang alkaline basalt(73 Ma) of the Wangshi Group. Both rocks show no negative Nb and Ta anomalies, but display E-MORB-like and OIB-like trace element distribution patterns, respectively. However, the Xiguanzhuang tholeiitic basalts have higher (87 Sr/86 Sr) and lower ε Nd(t)(0.7058,0.37~0.57) than the Daxizhuang alkaline basalts(0.7040,5.5~5.7). It is suggested that the former was formed as a result of interaction between asthenospheric melts and old-enriched lithosphere, whereas the latter represents asthenosphere-derived melts.The ε Nd(t) values in the studied magmas increase with decreasing age, consistent with upwelling of asthenosphere subsequent to the thinning of ancient lithosphere. This marks lithospheric thinning during Late Cretaceous-Early Cenozoic. Similar temporal variations in ε Nd(t) values are also observed for magmas in the western(120~100 Ma) and eastern(80~60 Ma) Liaoning province. This again attests to diachroneity of lithospheric thinning processes beneath the North China Craton.
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spelling curtin-20.500.11937-276762017-01-30T13:00:33Z Geochronology and Geochemistry of the Late Cretaceous Basalts in the Jiaolai Basin: Constraints on Lithospheric Thinning and Accretion Beneath North China Craton Kuang, Y. Pang, Chongjin Hong, L. Zhong, Y. Xu, Y. Ar-Ar dating Cretaceous basalt Jiaolai basin Geochemistry lithospheric thinning and accretion North China Craton Previous studies showed a heterogeneous temporal and spatial pattern of lithospheric thinning beneath North China Craton(NCC).The idea is mainly built on the diachronous eruption of the earliest asthenosphere-derived magmas in northern and southern NCC. In this study,we carried out Ar-Ar dating on the Xiguanzhuang tholeiitic basalt(the Jiaolai basin).40 Ar-39 Ar data show that it erupted at 96±3 Ma,thus belonging to the Qingshan Group,earlier than the Daxizhuang alkaline basalt(73 Ma) of the Wangshi Group. Both rocks show no negative Nb and Ta anomalies, but display E-MORB-like and OIB-like trace element distribution patterns, respectively. However, the Xiguanzhuang tholeiitic basalts have higher (87 Sr/86 Sr) and lower ε Nd(t)(0.7058,0.37~0.57) than the Daxizhuang alkaline basalts(0.7040,5.5~5.7). It is suggested that the former was formed as a result of interaction between asthenospheric melts and old-enriched lithosphere, whereas the latter represents asthenosphere-derived melts.The ε Nd(t) values in the studied magmas increase with decreasing age, consistent with upwelling of asthenosphere subsequent to the thinning of ancient lithosphere. This marks lithospheric thinning during Late Cretaceous-Early Cenozoic. Similar temporal variations in ε Nd(t) values are also observed for magmas in the western(120~100 Ma) and eastern(80~60 Ma) Liaoning province. This again attests to diachroneity of lithospheric thinning processes beneath the North China Craton. 2012 Journal Article http://hdl.handle.net/20.500.11937/27676 Zhongguo Kexueyuan Guangzhou Diqiu Huaxue Yanjiusuo restricted
spellingShingle Ar-Ar dating
Cretaceous basalt
Jiaolai basin
Geochemistry
lithospheric thinning and accretion
North China Craton
Kuang, Y.
Pang, Chongjin
Hong, L.
Zhong, Y.
Xu, Y.
Geochronology and Geochemistry of the Late Cretaceous Basalts in the Jiaolai Basin: Constraints on Lithospheric Thinning and Accretion Beneath North China Craton
title Geochronology and Geochemistry of the Late Cretaceous Basalts in the Jiaolai Basin: Constraints on Lithospheric Thinning and Accretion Beneath North China Craton
title_full Geochronology and Geochemistry of the Late Cretaceous Basalts in the Jiaolai Basin: Constraints on Lithospheric Thinning and Accretion Beneath North China Craton
title_fullStr Geochronology and Geochemistry of the Late Cretaceous Basalts in the Jiaolai Basin: Constraints on Lithospheric Thinning and Accretion Beneath North China Craton
title_full_unstemmed Geochronology and Geochemistry of the Late Cretaceous Basalts in the Jiaolai Basin: Constraints on Lithospheric Thinning and Accretion Beneath North China Craton
title_short Geochronology and Geochemistry of the Late Cretaceous Basalts in the Jiaolai Basin: Constraints on Lithospheric Thinning and Accretion Beneath North China Craton
title_sort geochronology and geochemistry of the late cretaceous basalts in the jiaolai basin: constraints on lithospheric thinning and accretion beneath north china craton
topic Ar-Ar dating
Cretaceous basalt
Jiaolai basin
Geochemistry
lithospheric thinning and accretion
North China Craton
url http://hdl.handle.net/20.500.11937/27676