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The Formation of Highly Positive δ34S Values in Late Devonian Mudstones: Microscale Analysis of Pyrite (δ34S) and Barite (δ34S, δ18O) in the Canol Formation (Selwyn Basin, Canada)
Swedish Museum of Natural History, Department of Geology. (Nordsim)ORCID iD: 0000-0003-2227-577X
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2022 (English)In: Frontiers in Earth Science, E-ISSN 2296-6463, Vol. 9, article id 784824Article in journal (Refereed) Published
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2022. Vol. 9, article id 784824
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Geochemistry
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The changing Earth
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URN: urn:nbn:se:nrm:diva-4961DOI: 10.3389/feart.2021.784824OAI: oai:DiVA.org:nrm-4961DiVA, id: diva2:1717207
Available from: 2022-12-07 Created: 2022-12-07 Last updated: 2023-08-28Bibliographically approved

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Whitehouse, Martin J.
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