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Very high-pressure orogenic garnet peridotites
Mantle-derived garnet peridotites are a minor component in many very high-pressure metamorphic terranes that formed during continental subduction and collision. Some of these mantle rocks contain trace amounts of zircon and micrometer-sized inclusions. The constituent minerals exhibit pre- and posts...
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| Main Authors: | , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2007
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC1890456/ https://ncbi.nlm.nih.gov/pubmed/17519341 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0607300104 |
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