Hydrothermal silicification and hypogene dissolution of an exhumed Neoproterozoic carbonate sequence in Brazil: Insights from fluid inclusion microthermometry and silicon‐oxygen isotopes-Reference-Cited by-同舟云学术

Hydrothermal silicification and hypogene dissolution of an exhumed Neoproterozoic carbonate sequence in Brazil: Insights from fluid inclusion microthermometry and silicon‐oxygen isotopes

Published:2023-01-11 Issue: Volume: Page:
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Research

Author:

Pisani Luca¹^ORCID,Koltai Gabriella²,Dublyansky Yuri²,Kleine Barbara I.³⁴,Whitehouse Martin J.⁵,Skrzypek Etienne⁶,Carbone Cristina⁷,Spötl Christoph²,Antonellini Marco¹,Bezerra Francisco H.⁸,De Waele Jo¹

Affiliation:

1. Department of Biological, Geological and Environmental Sciences Bologna University Bologna Italy

2. Institute of Geology University of Innsbruck Innsbruck Austria

3. Nordic Volcanological Center, Institute of Earth Sciences University of Iceland Reykjavik Iceland

4. GeoZentrum Nordbayern Friedrich‐Alexander‐Universität Erlangen‐Nürnberg Erlangen Germany

5. Swedish Museum of Natural History Stockholm Sweden

6. Institute of Earth Sciences, NAWI Graz Geozentrum, Petrology and Geochemistry University of Graz Graz Austria

7. DISTAV, Dipartimento di Scienze della Terra, dell'Ambiente e della Vita Università di Genova Genova Italy

8. Programa de Pós‐Graduação em Geodinâmica e Geofísica Federal University of Rio Grande Do Norte Natal Brazil

Funder

Shell Brasil

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12748

Reference137 articles.

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3. Late Ediacaran syn-rift/post-rift transition and related fault-driven hydrothermal systems in the Anti-Atlas Mountains, Morocco

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