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Oxygen isotopes in ophicalcites: an ever-lasting controversy?
Tectono-sedimentary breccias, known as ophicalcites, overlie serpentinised peridotites at a Jurassic ocean–continent transition along the Penninic-Austroalpine transition in the Eastern Alps of Switzerland. Deformation of the exhumed mantle rocks and breccia formation occurred under decreasing tempe...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Springer Berlin Heidelberg
2020
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7870598/ https://www.ncbi.nlm.nih.gov/pubmed/33603566 http://dx.doi.org/10.1007/s00531-020-01934-5 |