A reliable analytical procedure to determine the carbon isotopic signature of CO 2 -bearing COH flui...
A reliable analytical procedure to determine the carbon isotopic signature of CO 2 -bearing COH fluids generated in petrological experiments
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English
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The ratio of stable carbon isotopes, δ13C, serves as a fundamental tracer for geological processes. Experiments aiming to replicate isotopic exchange between carbon reservoirs encounter significant analytical challenges due to the limited sample size and issues related to sampling, particularly when dealing with volatile species. Here we present a...
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A reliable analytical procedure to determine the carbon isotopic signature of CO 2 -bearing COH fluids generated in petrological experiments
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TN_cdi_crossref_primary_10_5194_ejm_37_25_2025
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_crossref_primary_10_5194_ejm_37_25_2025
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1617-4011
E-ISSN
1617-4011
DOI
10.5194/ejm-37-25-2025