Combined use of conventional and clumped carbonate stable isotopes to identify hydrothermal isotopic alteration in cave walls

Alteration of conventional carbonate stable isotopes (δ(18)O, δ(13)C) in cave walls has been shown to be a useful tool to identify cave formation driven by deep-seated processes, i.e., hypogene karstification. If combined with a prior information on the paleowater stable isotope composition, further...

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Detalles Bibliográficos
Autores principales: Temovski, Marjan, Rinyu, László, Futó, István, Molnár, Kata, Túri, Marianna, Demény, Attila, Otoničar, Bojan, Dublyansky, Yuri, Audra, Philippe, Polyak, Victor, Asmerom, Yemane, Palcsu, László
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9163031/
https://www.ncbi.nlm.nih.gov/pubmed/35654959
http://dx.doi.org/10.1038/s41598-022-12929-4

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9163031/
https://www.ncbi.nlm.nih.gov/pubmed/35654959
http://dx.doi.org/10.1038/s41598-022-12929-4

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