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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...
| Autores principales: | , , , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2022
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| Materias: | |
| 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 |