Postcollisional mafic igneous rocks record crust-mantle interaction during continental deep subduction

Findings of coesite and microdiamond in metamorphic rocks of supracrustal protolith led to the recognition of continental subduction to mantle depths. The crust-mantle interaction is expected to take place during subduction of the continental crust beneath the subcontinental lithospheric mantle wedg...

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Detalles Bibliográficos
Autores principales: Zhao, Zi-Fu, Dai, Li-Qun, Zheng, Yong-Fei
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2013
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3849635/
https://www.ncbi.nlm.nih.gov/pubmed/24301173
http://dx.doi.org/10.1038/srep03413

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3849635/
https://www.ncbi.nlm.nih.gov/pubmed/24301173
http://dx.doi.org/10.1038/srep03413

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