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Article: Early Devonian (415−400 Ma) A-type granitoids and diabases in the Wuyishan, eastern Cathaysia: A signal of crustal extension coeval with the separation of South China from Gondwana

TitleEarly Devonian (415−400 Ma) A-type granitoids and diabases in the Wuyishan, eastern Cathaysia: A signal of crustal extension coeval with the separation of South China from Gondwana
Authors
KeywordsA-type granites
absolute age
Asia
Cathaysia
China
Issue Date2020
PublisherGeological Society of America. The Journal's web site is located at https://pubs.geoscienceworld.org/gsabulletin
Citation
GSA Bulletin, 2020, Epub 2020-03-18 How to Cite?
AbstractThe evolution of the South China continental crust and its linkage to the assembly and rifting of eastern Gondwana are key issues in the understanding of the early Paleozoic evolution of eastern Asia. We report U-Pb zircon ages and geochemical and Lu-Hf isotopic data for the South Fufang and Yingshang granitoids and the Mayuan diabases from the Wuyishan of eastern South China. The zircons yielded U-Pb ages of ca. 414−404 and ca. 409−401 Ma for the granitoids and diabases, respectively. Petrographic and geochemical features indicate that the granitoids are peraluminous A-type granites, expressed by high Ga/Al ratios and high Zr, Nb, Ce, Y, and rare earth element contents. They show negative zircon εHf(t) values (−15.4 to −5.8), consistent with the derivation from a crustal source. The granitoids likely originated from partial melting of dry granulite residues in the lower crust. The diabases show depletion in Ti, and negative correlations between FeOt and Mg#, and SiO2 and TiO2/FeOt, reflecting clinopyroxene, olivine, and Fe-Ti oxide fractionation. Their negative zircon εHf(t) values (−4.5 to −0.4) indicate an ancient enriched-mantle origin. The diabases likely originated from partial melting of a sub-continental lithospheric mantle. We interpret these A-type granitoids and diabases as post-orogenic, formed during extensional collapse of thickened crust. Their generation indicates that South China experienced crustal extension during the Early Devonian. The extension occurred coevally with global rifting that led to the separation of the continental blocks of eastern Asia from eastern Gondwana, which was associated with the Early Devonian opening of the paleo−Tethys Ocean.
Persistent Identifierhttp://hdl.handle.net/10722/283721
ISSN
2019 Impact Factor: 3.558
2015 SCImago Journal Rankings: 2.299
ISI Accession Number ID

 

DC FieldValueLanguage
dc.contributor.authorXIN, Y-
dc.contributor.authorLi, J-
dc.contributor.authorRatschbacher, L-
dc.contributor.authorZhao, G-
dc.contributor.authorZHANG, Y-
dc.contributor.authorDONG, S-
dc.contributor.authorXIA, X-
dc.contributor.authorYU, Y-
dc.date.accessioned2020-07-03T08:23:10Z-
dc.date.available2020-07-03T08:23:10Z-
dc.date.issued2020-
dc.identifier.citationGSA Bulletin, 2020, Epub 2020-03-18-
dc.identifier.issn0016-7606-
dc.identifier.urihttp://hdl.handle.net/10722/283721-
dc.description.abstractThe evolution of the South China continental crust and its linkage to the assembly and rifting of eastern Gondwana are key issues in the understanding of the early Paleozoic evolution of eastern Asia. We report U-Pb zircon ages and geochemical and Lu-Hf isotopic data for the South Fufang and Yingshang granitoids and the Mayuan diabases from the Wuyishan of eastern South China. The zircons yielded U-Pb ages of ca. 414−404 and ca. 409−401 Ma for the granitoids and diabases, respectively. Petrographic and geochemical features indicate that the granitoids are peraluminous A-type granites, expressed by high Ga/Al ratios and high Zr, Nb, Ce, Y, and rare earth element contents. They show negative zircon εHf(t) values (−15.4 to −5.8), consistent with the derivation from a crustal source. The granitoids likely originated from partial melting of dry granulite residues in the lower crust. The diabases show depletion in Ti, and negative correlations between FeOt and Mg#, and SiO2 and TiO2/FeOt, reflecting clinopyroxene, olivine, and Fe-Ti oxide fractionation. Their negative zircon εHf(t) values (−4.5 to −0.4) indicate an ancient enriched-mantle origin. The diabases likely originated from partial melting of a sub-continental lithospheric mantle. We interpret these A-type granitoids and diabases as post-orogenic, formed during extensional collapse of thickened crust. Their generation indicates that South China experienced crustal extension during the Early Devonian. The extension occurred coevally with global rifting that led to the separation of the continental blocks of eastern Asia from eastern Gondwana, which was associated with the Early Devonian opening of the paleo−Tethys Ocean.-
dc.languageeng-
dc.publisherGeological Society of America. The Journal's web site is located at https://pubs.geoscienceworld.org/gsabulletin-
dc.relation.ispartofGSA Bulletin-
dc.subjectA-type granites-
dc.subjectabsolute age-
dc.subjectAsia-
dc.subjectCathaysia-
dc.subjectChina-
dc.titleEarly Devonian (415−400 Ma) A-type granitoids and diabases in the Wuyishan, eastern Cathaysia: A signal of crustal extension coeval with the separation of South China from Gondwana-
dc.typeArticle-
dc.identifier.emailZhao, G: gzhao@hku.hk-
dc.identifier.authorityZhao, G=rp00842-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1130/B35412.1-
dc.identifier.hkuros310696-
dc.identifier.volumeEpub 2020-03-18-
dc.identifier.isiWOS:000588959000005-
dc.publisher.placeUnited States-
dc.identifier.issnl0016-7606-

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