Closing in on the oxygen isotopic fractionation factor between calcite and water using natural carbonates

dc.contributor.authorBreitenbach, Sebastian F.M.en_NZ
dc.contributor.authorHartland, Adamen_NZ
dc.contributor.authorBrall, Niels S.en_NZ
dc.contributor.authorSharp, Warren D.en_NZ
dc.contributor.authorGazquez, Fernandoen_NZ
dc.coverage.spatialConference held Vienna, Austriaen_NZ
dc.date.accessioned2019-10-21T20:31:27Z
dc.date.available2019en_NZ
dc.date.available2019-10-21T20:31:27Z
dc.date.issued2019en_NZ
dc.description.abstractThe oxygen isotopic fractionation between water and calcite is the cornerstone for estimating the formation temperature of calcite [1, 2, 3]. The oxygen isotope thermometer is one of the most valuable tools in geothermometry, palaeoclimatology and palaeoceanography
dc.format.mimetypeapplication/pdf
dc.identifier.citationBreitenbach, S. F. M., Hartland, A., Brall, N. S., Sharp, W. D., & Gazquez, F. (2019). Closing in on the oxygen isotopic fractionation factor between calcite and water using natural carbonates. In European Geosciences Union General Assembly 2019 (Vol. 21, pp. 6196–6196). Conference held Vienna, Austria.en
dc.identifier.urihttps://hdl.handle.net/10289/12986
dc.language.isoen
dc.relation.isPartOfEuropean Geosciences Union General Assembly 2019en_NZ
dc.relation.urihttps://meetingorganizer.copernicus.org/EGU2019/EGU2019-6196.pdfen_NZ
dc.rights© Author(s) 2019. CC Attribution 4.0 license.
dc.titleClosing in on the oxygen isotopic fractionation factor between calcite and water using natural carbonatesen_NZ
dc.typeConference Contribution
dspace.entity.typePublication
pubs.begin-page6196
pubs.end-page6196
pubs.volume21en_NZ

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