Stable oxygen and carbon isotope compositions of garnet and carbonates in metamorphic aureoles

Creator(s):
Ramos, Evan; ORCID: 0000000229192865
Abstract:
This dataset presents the stable oxygen isotope composition of garnets and the stable carbon isotope composition of carbonates in a metamorphic aureole. These measurements were used to understand the hydrothermal history of a skarn in the Sierra Nevada batholith of California. Whereas the oxygen isotope composition of garnets directly trace the fluids from which they crystallize, the oxygen and stable carbon isotope compositions of carbonates (calcite, limestone, marble) in metamorphic environments can be used to determine the drivers of decarbonation reactions (i.e. those that form calc-silicate minerals that comprise skarns).
How to cite this dataset:
Ramos, E., 2021. Stable oxygen and carbon isotope compositions of garnet and carbonates in metamorphic aureoles, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111852. Accessed 2021-09-20.
DOI Creation Date:
2021-01-20
Related
Publication(s):
Ramos, Evan J., Hesse, Marc A., Barnes, Jaime D., Jordan, Jacob S., Lackey, Jade Star, (2018), "Reevaluating fluid sources during skarn formation: An assessment of the Empire Mountain skarn, Sierra Nevada, USA." Geochemistry, Geophysics, Geosystems, 19(10): 3657-3672.
License:
Creative Commons Attribution-ShareAlike 4.0 International [CC BY-SA 4.0]
Funding source(s):
National Science Foundation: 1338842
Keyword(s):
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Empire Mountain, Mineral King, Sierra Nevada, California
User Contributed Keyword(s):
garnet, skarn, decarbonation, stable isotope geochemistry
Data Available On:
2021-01-21
Resource Type:
Dataset
Download File(s)
File Name
File Size
File Checksum
1852-1_Ramos_oxygen_carbon_isotope_Sierra_Nevada_2021.xls
150 KB

Related Information
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