In situ Rb/Sr geochronology and stable isotope geochemistry evidence for Neoproterozoic and Paleozoic fracture-hosted fluid flow and microbial activity in Paleoproterozoic basement, SW Sweden.
SND-ID: 2023-19-1. Version: 1. DOI: https://doi.org/10.5878/qa59-k342
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Creator/Principal investigator(s)
Henrik Drake - Linnaeus University, Department of Biology and Environmental Science
Research principal
Linnaeus University - Department of Biology and Environmental Science
Description
Raw and reduced data from analysis of C, O, S, Sr, Rb/Sr isotope systems in geological materials, along with organic geochemistry data. The tables include both data from unknowns and reference materials.
Data contains personal data
No
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Geographic spread
Geographic location: Sweden
Responsible department/unit
Department of Biology and Environmental Science
Research area
Earth and related environmental sciences (Standard för svensk indelning av forskningsämnen 2011)
Geosciences, multidisciplinary (Standard för svensk indelning av forskningsämnen 2011)
Natural sciences (Standard för svensk indelning av forskningsämnen 2011)
Geology (Standard för svensk indelning av forskningsämnen 2011)
Geochemistry (Standard för svensk indelning av forskningsämnen 2011)
Microbiology (Standard för svensk indelning av forskningsämnen 2011)
Keywords
Henrik Drake, Mikael Tillberg, Manuel Reinhardt, Martin Whitehouse, Ellen Kooijman, In situ Rb/Sr geochronology and stable isotope geochemistry evidence for Neoproterozoic and Paleozoic fracture-hosted fluid flow and microbial activity in Paleoproterozoic basement, SW Sweden, Geochemistry Geophysics, Geosystems, 24(5), e2023GC010892, 2023.
DOI:
https://doi.org/10.1029/2023GC010892
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