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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...
| Autores principales: | , , , , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2020
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| 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 |