Ongoing formation of felsic lower crustal channel by relamination in Zagros collision zone revealed from regional tomography

Complex interaction of rheologically contrasting layers within the lithosphere during the collision of continental plates leads to active faulting, which represents a serious hazard to the population and infrastructure. One of the collision scenarios presumes the existence of a middle-lower crustal...

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Detalles Bibliográficos
Autores principales: Talebi, Amir, Koulakov, Ivan, Moradi, Ali, Rahimi, Habib, Gerya, Taras
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7237424/
https://www.ncbi.nlm.nih.gov/pubmed/32427975
http://dx.doi.org/10.1038/s41598-020-64946-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7237424/
https://www.ncbi.nlm.nih.gov/pubmed/32427975
http://dx.doi.org/10.1038/s41598-020-64946-w

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