Microdiamond in a low-grade metapelite from a Cretaceous subduction complex, western Kyushu, Japan

Microdiamonds in metamorphic rocks are a signature of ultrahigh-pressure (UHP) metamorphism that occurs mostly at continental collision zones. Most UHP minerals, except coesite and microdiamond, have been partially or completely retrogressed during exhumation; therefore, the discovery of coesite and...

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Detalles Bibliográficos
Autores principales: Nishiyama, Tadao, Ohfuji, Hiroaki, Fukuba, Kousuke, Terauchi, Masami, Nishi, Ukyo, Harada, Kazuki, Unoki, Kouhei, Moribe, Yousuke, Yoshiasa, Akira, Ishimaru, Satoko, Mori, Yasushi, Shigeno, Miki, Arai, Shoji
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/PMC7363827/
https://www.ncbi.nlm.nih.gov/pubmed/32669632
http://dx.doi.org/10.1038/s41598-020-68599-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7363827/
https://www.ncbi.nlm.nih.gov/pubmed/32669632
http://dx.doi.org/10.1038/s41598-020-68599-7

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