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Publikováno v:
Journal of GEOsciences. :3-19
*Corr esponding author A strongly layered garnet pyroxenite, consisting of cm-scale layers of garnetite, garnet orthopyroxenite, garnet clinopyroxenite, and websterite, occurs in the Biskupice garnet peridotite, which is located in migmatitic gneiss
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee4f8b048bb177cb2ca6489e58181289
https://doi.org/10.3190/jgeosci.131
https://doi.org/10.3190/jgeosci.131
