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The thermal imprint of continental breakup during the formation of the South China Sea

dc.contributor.authorNirrengarten, Michael
dc.contributor.authorMohn, Geoffroy
dc.contributor.authorSchito, Andrea
dc.contributor.authorCorrado, Sveva
dc.contributor.authorGutiérrez-García, Laura
dc.contributor.authorBowden, Stephen
dc.contributor.authorDespinois, Frank
dc.date.accessioned2020-01-23T11:10:04Z
dc.date.available2020-01-23T11:10:04Z
dc.date.issued2020-02-01
dc.identifier.citationNirrengarten , M , Mohn , G , Schito , A , Corrado , S , Gutiérrez-García , L , Bowden , S & Despinois , F 2020 , ' The thermal imprint of continental breakup during the formation of the South China Sea ' , Earth and Planetary Science Letters , vol. 531 , 115972 . https://doi.org/10.1016/j.epsl.2019.115972en
dc.identifier.issn0012-821X
dc.identifier.otherPURE: 149394663
dc.identifier.otherPURE UUID: 1e3f3865-7f0d-4f58-8886-bbba25d56668
dc.identifier.otherScopus: 85076247107
dc.identifier.otherWOS: 000510947100028
dc.identifier.urihttps://hdl.handle.net/2164/13573
dc.descriptionThis research used data provided by the International Ocean Discovery Program (IODP).We thanks the participants to IODP Expedition 367-368 as well as the captains and crew of the Joides Resolution. Seismic sections originate from the IODP Expedition 367/368/368X proceeding volume. Platte River Associates, Inc is thanked for providing an academic licence of BasinMod 2D. We acknowledge IODP France and ECORD for the support. Funding for this research was provided by Total SA R&D (J.N. Ferry). SAB gratefully acknowledges NERC award NE/R002576/1; Measuring Rates of Weathered Petroleum Accumulation, South China Sea.en
dc.language.isoeng
dc.relation.ispartofEarth and Planetary Science Lettersen
dc.rights© 2019 The Authors Published by Elsevier B.V. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).en
dc.subjectcontinental breakupen
dc.subjectthermal evolutionen
dc.subjectSE China distal marginen
dc.subjectIODPen
dc.subjectorganic petrographyen
dc.subjectRaman spectroscopyen
dc.subjectbiomarker analysisen
dc.subjectSE China Marginen
dc.subjectIODP 367-368en
dc.subjectRAMAN-SPECTRAen
dc.subjectEASTERN GULFen
dc.subjectCRUSTAL EXTENSIONen
dc.subjectCARBONACEOUS MATERIALen
dc.subjectORGANIC-MATTERen
dc.subjectMARGINen
dc.subjectEVOLUTIONen
dc.subjectSEDIMENTARY BASINSen
dc.subjectNEWFOUNDLANDen
dc.subjectHEAT-FLOWen
dc.subjectQE Geologyen
dc.subjectGeochemistry and Petrologyen
dc.subjectGeophysicsen
dc.subjectEarth and Planetary Sciences (miscellaneous)en
dc.subjectSpace and Planetary Scienceen
dc.subjectNatural Environment Research Council (NERC)en
dc.subjectNE/R002576/1en
dc.subject.lccQEen
dc.titleThe thermal imprint of continental breakup during the formation of the South China Seaen
dc.typeJournal articleen
dc.contributor.institutionUniversity of Aberdeen.Geology and Geophysicsen
dc.contributor.institutionUniversity of Aberdeen.Centre for Energy Transitionen
dc.description.statusPeer revieweden
dc.description.versionPublisher PDFen
dc.identifier.doihttps://doi.org/10.1016/j.epsl.2019.115972
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=85076247107&partnerID=8YFLogxKen
dc.identifier.vol531en


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