Metamorphic pressure variation in a coherent Alpine nappe challenges lithostatic pressure paradigm

Pressure–temperature–time paths obtained from minerals in metamorphic rocks allow the reconstruction of the geodynamic evolution of mountain ranges under the assumption that rock pressure is lithostatic. This lithostatic pressure paradigm enables converting the metamorphic pressure directly into the...

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Detalles Bibliográficos
Autores principales: Luisier, Cindy, Baumgartner, Lukas, Schmalholz, Stefan M., Siron, Guillaume, Vennemann, Torsten
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6800426/
https://www.ncbi.nlm.nih.gov/pubmed/31628316
http://dx.doi.org/10.1038/s41467-019-12727-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6800426/
https://www.ncbi.nlm.nih.gov/pubmed/31628316
http://dx.doi.org/10.1038/s41467-019-12727-z

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