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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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Bibliographic Details
Main Authors: Liou, J. G., Zhang, R. Y., Ernst, W. G.
Format: Artigo
Language:Inglês
Published: National Academy of Sciences 2007
Subjects:
Online Access: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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