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MORB melt metasomatism and deserpentinization in the peridotitic member of Variscan ophiolite: an example of the Braszowice-Brzeznica serpentinites (SW Poland)

Publications: Contribution to journalArticlePeer Reviewed

Original languageEnglish
Pages (from-to)147-164
Number of pages18
JournalJournal of Geosciences
Volume62
Issue number3
DOIs
Publication statusPublished - 2017

Funding

This paper was prepared as a part of the project of the National Science Centre of Poland ("Evolution of the serpentinitic members of ophiolites from Lower Silesia", DEC-2012/07/N/ST10/03934). Comments on the manuscript by two anonymous reviewers helped us to improve the manuscript. The authors are grateful to handling editor E. Jelinek for his helpful remarks. Comments and language correction of V. Janousek significantly improved this paper. Thanks go to K. Dymna, P. Matz (University of Wroclaw), F. Kiraly (University of Vienna) and M. Bukala (AGH University of Science and Technology) for their technical and analytical assistance.

Austrian Fields of Science 2012

  • 105105 Geochemistry
  • 105120 Petrology

Keywords

  • Variscan ophiolite
  • peridotitic member
  • MORB melt percolation
  • clinopyroxene
  • Braszowice-Brzeznica Massif
  • Bohemian Massif
  • MID-ATLANTIC RIDGE
  • CONTACT METAMORPHISM
  • MANTLE PERIDOTITES
  • OMAN OPHIOLITE
  • SOUTH ATLANTIC
  • WESTERN ALPS
  • ARC-BASIN
  • GEOCHEMISTRY
  • ANTIGORITE
  • SECTION
  • Bohemian massif
  • Braszowice-brzeźnica massif
  • Morb melt percolation
  • Peridotitic member
  • Clinopyroxene

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