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Fluid expulsion system and tectonic architecture of the incipient Cascadia convergent margin as revealed by Nd, Sr and stable isotope composition of mid-Eocene methane seep carbonates
Swedish Museum of Natural History, Department of Paleobiology.ORCID iD: 0000-0001-6281-100X
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2020 (English)In: Chemical Geology, Vol. 558, article id 119872Article in journal (Refereed) Published
Place, publisher, year, edition, pages
2020. Vol. 558, article id 119872
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Geology
Research subject
The changing Earth
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URN: urn:nbn:se:nrm:diva-3819OAI: oai:DiVA.org:nrm-3819DiVA, id: diva2:1500200
Available from: 2020-11-11 Created: 2020-11-11 Last updated: 2020-11-11Bibliographically approved

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https://doi.org/10.1016/j.chemgeo.2020.119872

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Jakubowicz, MichalKiel, Steffen
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