Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Małgorzata Ziobro-Mikrut"'
Autor:
Jacek Puziewicz, Sonja Aulbach, Magdalena Matusiak-Małek, Theodoros Ntaflos, Małgorzata Ziobro-Mikrut
The Hessian Depression in Germany represents the northern continuation of the Upper Rhine Graben and is known for Cenozoic alkaline basaltic lavas. Many of these carry peridotite xenoliths of mantle origin, which were studied mainly in the 80-ies of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01b43a3b6e492963495fa82404eb4f47
https://doi.org/10.5194/egusphere-egu23-2878
https://doi.org/10.5194/egusphere-egu23-2878
The 3.5-0.5 Ma Devès volcanic field is located in the “southern” mantle domain of the French Massif Central (MC), which originated by partial melting, likely followed by refertilization by melts from the upwelling asthenosphere [1, 2]. However,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0275c808f40de49d9f457dfbf086b84f
https://doi.org/10.5194/egusphere-egu23-14795
https://doi.org/10.5194/egusphere-egu23-14795
Autor:
Jacek Puziewicz, Sonja Aulbach, Mary-Alix Kaczmarek, Anna Kukuła, Theodoros Ntaflos, Magdalena Matusiak-Małek, Sylvin S. T. Tedonkenfack, Małgorzata Ziobro-Mikrut
The Wum maar is located in the Oku Volcanic group, part of continental sector of the Cameroon Volcanic Line (CVL) in west Africa, which consists of volcanoes active from Eocene to recent. The continental part of the CVL is located on the metamorphic-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::04a49f5402d9bf942d39f0fab9e3d441
https://doi.org/10.5194/egusphere-egu22-1865
https://doi.org/10.5194/egusphere-egu22-1865
Autor:
Małgorzata Ziobro-Mikrut, Jacek Puziewicz, Sonja Aulbach, Theodoros Ntaflos, Magdalena Matusiak-Małek
The 3.5-0.5 Ma Devès volcanic field consists mainly of nepheline basanite rocks. The underlying Variscan basement is a part of the western Moldanubian Zone (an allochton of the European Variscan orogen, probably the Gondwana margin). The Devès volc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::676ad13079f634465ef2c93c66df3ba3
https://doi.org/10.5194/egusphere-egu22-4351
https://doi.org/10.5194/egusphere-egu22-4351