Zobrazeno 1 - 10
of 10
pro vyhledávání: '"metasomatóza"'
Autor:
Zelinková, Tereza
English Abstract The Dunkelsteiner Wald granulite massif in Lower Austria belongs to the Gföhl unit of the Moldanubian zone of the Bohemian Massif. Predominant rocks are felsic granulites which in some places contain garnet pyroxenites and peridotit
Externí odkaz:
http://www.nusl.cz/ntk/nusl-388407
Autor:
Roman Skála, Jana Ďurišová, Šárka Křížová, Simona Kuboušková, Lukáš Krmíček, Jiří Adamovič, Claudia Teschner, Jaromír Ulrych, Miroslav Radoň
Publikováno v:
Lithos
Amphibole phenocrysts, xenocrysts and cumulate xenoliths from Cenozoic volcanic rocks of the Bohemian Massif (BM) belong to the magnesio-hastingsite–pargasite–kaersutite series. Their host rocks are mostly basaltic lavas, stocks, dykes and brecci
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5f2d6b49e990155205fe45853740a2a1
https://is.muni.cz/publication/1432338
https://is.muni.cz/publication/1432338
Autor:
Zelinková, Tereza
English Abstract The Dunkelsteiner Wald granulite massif in Lower Austria belongs to the Gföhl unit of the Moldanubian zone of the Bohemian Massif. Predominant rocks are felsic granulites which in some places contain garnet pyroxenites and peridotit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2186::00685a615692b0ed0ef3edb9e0c98752
http://www.nusl.cz/ntk/nusl-388407
http://www.nusl.cz/ntk/nusl-388407
Autor:
Krátký, Ondřej
English abstract The volcanic-hosted massive sulfide deposits (VHMS) represent one of the key deposit types in the modern world. Due to their polymetallic composition (Zn, Pb, Cu, Ag, Au and Sn in some cases) they are important source of the base met
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2186::e6e34b9351dc0cb8e4a94c97bc1f00cd
http://www.nusl.cz/ntk/nusl-345903
http://www.nusl.cz/ntk/nusl-345903
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
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
Akademický článek
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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
Autor:
Kovács, Andrea
Peridotites occuring in orogenic massifs provide important insights into geochemical processes of the Earth's upper mantle by providing direct evidence of mantle evolution throughout Earth history. It has been previously demostrated (e.g. Medaris et
Externí odkaz:
http://www.nusl.cz/ntk/nusl-295840
Autor:
Kovács, Andrea
Peridotites occuring in orogenic massifs provide important insights into geochemical processes of the Earth's upper mantle by providing direct evidence of mantle evolution throughout Earth history. It has been previously demostrated (e.g. Medaris et
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::8d7330d0f8ba9bde0f5daede865387fc
http://www.nusl.cz/ntk/nusl-295840
http://www.nusl.cz/ntk/nusl-295840