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...

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Detalles Bibliográficos
Autores principales: Bernoulli, Daniel, Weissert, Helmut
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2020
Materias:
Original Paper
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

Internet

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

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