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Conference Paper: Jiangnan Orogen in South China: developed from divergent double subduction?

TitleJiangnan Orogen in South China: developed from divergent double subduction?
Authors
Issue Date2014
PublisherInternational Association for Gondwana Research.
Citation
The 1st International Conference on Subduction, Volcanism and the Evolution of Oceanic and Continental Crust (SVEOCC 2014), Nadi, Fiji, 10-16 February 2014. In IAGR Conference Series 17, 2014, Abstract Volume, p. 65 How to Cite?
AbstractThe Jiangnan Orogen is considered as a continent-continent collisional belt resulting from the closure of a Meso-Neoproterozoic ocean separating the southeastern margin of the Yangtze Block from the northwestern margin of the Cathaysia Block. Recent data indicate the existence of early Neoproterozoic (1000-825 Ma) volcanic arc assemblages on both sides of the orogen, suggesting that the ocean lithosphere between the Yangtze and Cathaysia blocks must have undergone divergent double-sided subduction during the period of 1000-825 Ma, like what is happening in the Moluccan ocean plate within the Pacific Ocean. The divergent double subduction eventually resulted in the closure of the ocean basin …
Persistent Identifierhttp://hdl.handle.net/10722/201848

 

DC FieldValueLanguage
dc.contributor.authorZhao, G-
dc.date.accessioned2014-08-21T07:44:29Z-
dc.date.available2014-08-21T07:44:29Z-
dc.date.issued2014-
dc.identifier.citationThe 1st International Conference on Subduction, Volcanism and the Evolution of Oceanic and Continental Crust (SVEOCC 2014), Nadi, Fiji, 10-16 February 2014. In IAGR Conference Series 17, 2014, Abstract Volume, p. 65-
dc.identifier.urihttp://hdl.handle.net/10722/201848-
dc.description.abstractThe Jiangnan Orogen is considered as a continent-continent collisional belt resulting from the closure of a Meso-Neoproterozoic ocean separating the southeastern margin of the Yangtze Block from the northwestern margin of the Cathaysia Block. Recent data indicate the existence of early Neoproterozoic (1000-825 Ma) volcanic arc assemblages on both sides of the orogen, suggesting that the ocean lithosphere between the Yangtze and Cathaysia blocks must have undergone divergent double-sided subduction during the period of 1000-825 Ma, like what is happening in the Moluccan ocean plate within the Pacific Ocean. The divergent double subduction eventually resulted in the closure of the ocean basin …-
dc.languageeng-
dc.publisherInternational Association for Gondwana Research.-
dc.relation.ispartofIAGR Conference Series 17-
dc.rightsCreative Commons: Attribution 3.0 Hong Kong License-
dc.titleJiangnan Orogen in South China: developed from divergent double subduction?-
dc.typeConference_Paper-
dc.identifier.emailZhao, G: gzhao@hkucc.hku.hk-
dc.identifier.authorityZhao, G=rp00842-
dc.description.naturepublished_or_final_version-
dc.identifier.hkuros234190-
dc.identifier.volumeAbstract Volume-
dc.identifier.spage65-
dc.identifier.epage65-
dc.publisher.placeBeijing, China-

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