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Potential analytical interferences when measuring Tmax during temperature programmed pyrolysis of hydrothermally altered volcanoclastic sediment

dc.contributor.authorBowden, Stephen A.
dc.contributor.authorKobayashi, Yuino
dc.contributor.authorOffeh, Ogheneworo E.
dc.contributor.authorTsang, Man Yin
dc.contributor.authorYamamoto, Yuzuru
dc.contributor.institutionUniversity of Aberdeen.University of Aberdeenen
dc.contributor.institutionUniversity of Aberdeen.Geosciencesen
dc.date.accessioned2023-03-15T11:01:01Z
dc.date.available2023-03-15T11:01:01Z
dc.date.issued2023-02-10
dc.descriptionOpen Access via the CUP Agreement Funding Information: SAB acknowledges support by the Kobe University Strategic International Collaborative Research Grant Award and Daiwa Anglo-Japanese Foundation Small Grant, OEO acknowledges a PhD studentship sponsored by the Tertiary Education Trust Fund (Nigeria), MYT acknowledges the JSPS International Research Fellowship and the associated JSPS Grant-in-Aid (20F20773).en
dc.description.statusPeer revieweden
dc.format.extent11
dc.format.extent900488
dc.identifier229403690
dc.identifier8ceacf3c-261d-4185-9fe9-d01b9ea4abea
dc.identifier85148659011
dc.identifier.citationBowden, S A, Kobayashi, Y, Offeh, O E, Tsang, M Y & Yamamoto, Y 2023, 'Potential analytical interferences when measuring Tmax during temperature programmed pyrolysis of hydrothermally altered volcanoclastic sediment', Experimental Results, vol. 4, e5. https://doi.org/10.1017/exp.2023.3en
dc.identifier.doi10.1017/exp.2023.3
dc.identifier.issn2516-712X
dc.identifier.urihttps://hdl.handle.net/2164/20285
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=85148659011&partnerID=8YFLogxKen
dc.identifier.vol4en
dc.language.isoeng
dc.relation.ispartofExperimental Resultsen
dc.subjectRock-Evalen
dc.subjecttemperature programmed pyrolysisen
dc.subjectthermal maturityen
dc.subjectTmaxen
dc.subjectvolcanic sedimenten
dc.subjectQE Geologyen
dc.subjectGeneralen
dc.subject.lccQEen
dc.titlePotential analytical interferences when measuring Tmax during temperature programmed pyrolysis of hydrothermally altered volcanoclastic sedimenten
dc.typeJournal articleen

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