Mariana-type ophiolites constrain the establishment of modern plate tectonic regime during Gondwana assembly

Initiation of Mariana-type oceanic subduction zones requires rheologically strong oceanic lithosphere, which developed through secular cooling of Earth’s mantle. Here, we report a 518 Ma Mariana-type subduction initiation ophiolite from northern Tibet, which, along with compilation of similar ophiol...

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Detalles Bibliográficos
Autores principales: Yao, Jinlong, Cawood, Peter A., Zhao, Guochun, Han, Yigui, Xia, Xiaoping, Liu, Qian, Wang, Peng
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8263587/
https://www.ncbi.nlm.nih.gov/pubmed/34234127
http://dx.doi.org/10.1038/s41467-021-24422-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8263587/
https://www.ncbi.nlm.nih.gov/pubmed/34234127
http://dx.doi.org/10.1038/s41467-021-24422-z

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