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Graphite as an electrically conductive indicator of ancient crustal-scale fluid flow within mineral systems

dc.contributor.authorMurphy, Benjamin
dc.contributor.authorHuizenga, Jan Marten
dc.contributor.authorBedrosian, Paul
dc.date.accessioned2022-07-25T07:14:47Z
dc.date.available2022-07-25T07:14:47Z
dc.date.created2022-07-22T19:16:37Z
dc.date.issued2022
dc.identifier.citationEarth and Planetary Science Letters. 2022, 594, 117700.en_US
dc.identifier.issn0012-821X
dc.identifier.urihttps://hdl.handle.net/11250/3008098
dc.language.isoengen_US
dc.titleGraphite as an electrically conductive indicator of ancient crustal-scale fluid flow within mineral systemsen_US
dc.title.alternativeGraphite as an electrically conductive indicator of ancient crustal-scale fluid flow within mineral systemsen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersion
dc.source.pagenumber9en_US
dc.source.journalEarth and Planetary Science Lettersen_US
dc.identifier.doidoi.org/10.1016/j.epsl.2022.117700
dc.identifier.cristin2039147
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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