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Revealing the climate of snowball Earth from Δ(17)O systematics of hydrothermal rocks
The oxygen isotopic composition of hydrothermally altered rocks partly originates from the interacting fluid. We use the triple oxygen isotope composition ((17)O/(16)O, (18)O/(16)O) of Proterozoic rocks to reconstruct the (18)O/(16)O ratio of ancient meteoric waters. Some of these waters have origin...
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| Publicado no: | Proc Natl Acad Sci U S A |
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| Main Authors: | , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2015
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4418898/ https://ncbi.nlm.nih.gov/pubmed/25870269 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1422887112 |
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