Petrology of ultramafic lamprophyres from the Beaver Lake area of Eastern Antarctica and their relation to the breakup of Gondwanaland

Mesozoic melilite-bearing ultramafic lamprophyres are developed as sill, dyke and plug-like intrusive bodies in the East Antarctic Beaver Lake area. They consist of varying amounts of olivine, melilite, phlogopite, nepheline, titanomagnetite and perovskite as major phases, accompanied by minor amoun...

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Bibliographic Details
Published in:Mineralogy and Petrology
Main Authors: Melzer, S., Andronikov, A. V., Foley, S. F.
Other Authors: Department of Geological Sciences, University of Michigan, Ann Arbor, Mi, U.S.A., US, Projektbereich 4.1, Geoforschungszentrum Potsdam, Potsdam, Germany, DE, Institut für Geologische Wissenschaften, Universität Greifswald, Greifswald, Germany, DE, Ann Arbor
Format: Article in Journal/Newspaper
Language:English
Published: Springer-Verlag; Springer-Verlag Wien 2002
Subjects:
Online Access:http://hdl.handle.net/2027.42/42462
https://doi.org/10.1007/s007100200011