Kyanite eclogites and high-Mg garnet pyroxenites from the Czech Bohemian Massif were originally formed as cumulative gabbros

0054798 - GLÚ 2007 JP eng A - Abstract
Obata, M. - Svojtka, Martin - Christy, A. G.
Kyanite eclogites and high-Mg garnet pyroxenites from the Czech Bohemian Massif were originally formed as cumulative gabbros.
[Eklogity s kyanitem a vysoce hořečnaté granátické pyroxenity z Českého masivu vzniklé z kumulativních gaber.]
Japan Geoscience Union Meeting 2006. Conference Abstracts. -: Japan Geoscience Union, 2006. s. 104-104.
[Japan Geoscience Union Meeting 2006. 14.05.2006-18.05.2006, Chiba]
R&D Projects: GA MŠMT ME 679
Institutional research plan: CEZ:AV0Z30130516
Keywords : gabbro * kyanite * eclogite * Bohemian Massif
Subject RIV: DB - Geology ; Mineralogy

We present new data of whole-rock major and trace element analyses of three kyanite eclogites from the Nove Dvory garnet peridotite and demonstrate that these were all gabbroic origin.
Permanent Link: http://hdl.handle.net/11104/0142736