![Hier klicken, um den Treffer aus der Auswahl zu entfernen](images/unchecked.gif) |
Titel |
The modal mantle metasomatism in the NE part of the Cenozoic Central European Volcanic Province: the example of the Wołek basanite (SW Poland) |
VerfasserIn |
M. Nowak, J. Puziewicz, M. Gregoire, A. Muszynski |
Konferenz |
EGU General Assembly 2012
|
Medientyp |
Artikel
|
Sprache |
Englisch
|
Digitales Dokument |
PDF |
Erschienen |
In: GRA - Volume 14 (2012) |
Datensatznummer |
250066035
|
|
|
|
Zusammenfassung |
The Cenozoic lava occurrences in SW Poland belong to the Central European Volcanic
Province (CEVP). In some of them (ca.10) mantle xenoliths were recognized. Most of
xenoliths show no signs of modal metasomatism (Blusztajn and Shimizu 1994,
Matusiak-Małek et al. 2010, Puziewicz et al. 2011). One of the rare exposures with
amphibole-bearing peridotite xenoliths in SW Poland is the Wołek Hill basanite. It is located
about 100 km south-west of Wrocław (Nowak et al. 2010) in the Złotoryja volcanic field
(Matusiak-Małek et al. 2010).
Peridotite xenoliths from Wołek ( |
|
|
|
|