The major-ion composition of Cenozoic seawater: the past 36 million years from fluid inclusions in marine halite

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dc.contributor.authorBrennan, STen_AU
dc.contributor.authorLowenstein, TKen_AU
dc.contributor.authorCendón, DIen_AU
dc.date.accessioned2015-09-28T05:47:49Zen_AU
dc.date.available2015-09-28T05:47:49Zen_AU
dc.date.issued2013-10-01en_AU
dc.date.statistics2015-09-16en_AU
dc.description.abstractFluid inclusions from ten Cenozoic (Eocene-Miocene) marine halites are used to quantify the major-ion composition (Mg2+, Ca2+, K+, Na+, SO42-, and Cl-) of seawater over the past 36 My. Criteria used to determine a seawater origin of the halites include: (1) stratigraphic, sedimentologic, and paleontologic observations; (2) Br- in halite; (3) delta S-34 of sulfate minerals; (4) Sr-87/Sr-86 of carbonates and sulfates; and (5) fluid inclusion brine compositions and evaporation paths, which must overlap from geographically separated basins of the same age to confirm a "global" seawater chemical signal. © 2013, American Journal of Science.en_AU
dc.identifier.citationBrennan, S. T., Lowenstein, T. K., & Cendón, D. I.(2013). The major-ion composition of Cenozoic seawater: the past 36 million years from fluid inclusions in marine halite. American Journal of Science, 313(8), 713-775. doi:10.2475/08.2013.01en_AU
dc.identifier.govdoc6071en_AU
dc.identifier.issn1945-425Xen_AU
dc.identifier.issue8en_AU
dc.identifier.journaltitleAmerican Journal of Scienceen_AU
dc.identifier.pagination713-775en_AU
dc.identifier.urihttp://dx.doi.org/10.2475/08.2013.01en_AU
dc.identifier.urihttp://apo.ansto.gov.au/dspace/handle/10238/6226en_AU
dc.identifier.volume313en_AU
dc.language.isoenen_AU
dc.publisherAmerican Journal Scienceen_AU
dc.subjectCenozoic Eraen_AU
dc.subjectEvaporitesen_AU
dc.subjectStratigraphyen_AU
dc.subjectSea levelen_AU
dc.subjectHydrologyen_AU
dc.subjectSulfate mineralsen_AU
dc.titleThe major-ion composition of Cenozoic seawater: the past 36 million years from fluid inclusions in marine haliteen_AU
dc.typeJournal Articleen_AU
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