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Autor:
Bubal, Jan
Calcic-iron skarns are one of the characteristic part of the regional metamorphic complexes of the Bohemian Massif. Their mineral assemblages, structures and significant enrichment of Ca, Al and Fe were previously interpreted to be primary (exhalatio
Externí odkaz:
http://www.nusl.cz/ntk/nusl-321074
Publikováno v:
Geoconservation Research; Jun2023, Vol. 6 Issue 1, p98-113, 16p
Autor:
Bubal, Jan
Calcic-iron skarns are one of the characteristic part of the regional metamorphic complexes of the Bohemian Massif. Their mineral assemblages, structures and significant enrichment of Ca, Al and Fe were previously interpreted to be primary (exhalatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0ca8aa6ba07f1f94cd0f3281853abb3e
http://www.nusl.cz/ntk/nusl-486975
http://www.nusl.cz/ntk/nusl-486975
Autor:
Bubal, Jan
ENGLISH SUMMARY MINERAL ASSEMBLAGES AND CONDITIONS OF ORIGIN OF METAMORPHIC SKARNS IN THE BOHEMIAN MASSIF Calcic-iron skarns are a characteristic rock type of regional metamorphic complexes wirkude. In the Bohemian Massif, characteristic enrichment i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2186::425d92ef608e7ad952940de96d82cfd9
http://www.nusl.cz/ntk/nusl-314749
http://www.nusl.cz/ntk/nusl-314749