About: Garnet Breakdown, Symplectite Formation and Melting in Basanite-hosted Peridotite Xenoliths from Zinst (Bavaria, Bohemian Massif)     Goto   Sponge   NotDistinct   Permalink

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Description
  • Complex, symplectite-bearing pseudomorphs after garnet recently found in unique basanite-hosted peridotite xenoliths from Zinst, Bavaria, allow the study of the interaction between garnet peridotite and melts or fluids both prior to entrainment of the xenoliths and during their ascent. Based on microstructures and crystallographic fabric, and major and trace element mineral chemistry, four distinct concentric zones were defined in various types of pseudomorph: Zone I, coarse-grained (1 mm) aggregate of orthopyroxene + clinopyroxene + spinel with a granular structure; Zone II, fine- to medium-grained (order of 10-100 mu m) orthopyroxene + spinel symplectite; Zone III, fine-grained (5-300 mu m), radially fibrous orthopyroxene + spinel symplectite with interstitial anorthite; Zone IV, ultrafine-grained (1 mu m) orthopyroxene + spinel + anorthite symplectite with an internal domain substructure. Zones III and IV have bulk compositions of pyrope-rich garnet.
  • Complex, symplectite-bearing pseudomorphs after garnet recently found in unique basanite-hosted peridotite xenoliths from Zinst, Bavaria, allow the study of the interaction between garnet peridotite and melts or fluids both prior to entrainment of the xenoliths and during their ascent. Based on microstructures and crystallographic fabric, and major and trace element mineral chemistry, four distinct concentric zones were defined in various types of pseudomorph: Zone I, coarse-grained (1 mm) aggregate of orthopyroxene + clinopyroxene + spinel with a granular structure; Zone II, fine- to medium-grained (order of 10-100 mu m) orthopyroxene + spinel symplectite; Zone III, fine-grained (5-300 mu m), radially fibrous orthopyroxene + spinel symplectite with interstitial anorthite; Zone IV, ultrafine-grained (1 mu m) orthopyroxene + spinel + anorthite symplectite with an internal domain substructure. Zones III and IV have bulk compositions of pyrope-rich garnet. (en)
Title
  • Garnet Breakdown, Symplectite Formation and Melting in Basanite-hosted Peridotite Xenoliths from Zinst (Bavaria, Bohemian Massif)
  • Garnet Breakdown, Symplectite Formation and Melting in Basanite-hosted Peridotite Xenoliths from Zinst (Bavaria, Bohemian Massif) (en)
skos:prefLabel
  • Garnet Breakdown, Symplectite Formation and Melting in Basanite-hosted Peridotite Xenoliths from Zinst (Bavaria, Bohemian Massif)
  • Garnet Breakdown, Symplectite Formation and Melting in Basanite-hosted Peridotite Xenoliths from Zinst (Bavaria, Bohemian Massif) (en)
skos:notation
  • RIV/00216224:14310/13:00072496!RIV14-MSM-14310___
http://linked.open...avai/predkladatel
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(EE2.3.20.0052), P(GA205/09/1170), S
http://linked.open...iv/cisloPeriodika
  • 8
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 76179
http://linked.open...ai/riv/idVysledku
  • RIV/00216224:14310/13:00072496
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • garnet; symplectite; kelyphite; xenolith; melting; metasomatism; lithospheric mantle; Eger Rift; Bohemian Massif (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • GB - Spojené království Velké Británie a Severního Irska
http://linked.open...ontrolniKodProRIV
  • [8830554FDB79]
http://linked.open...i/riv/nazevZdroje
  • Journal of Petrology
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http://linked.open...ichTvurcuVysledku
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http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 54
http://linked.open...iv/tvurceVysledku
  • Ackerman, Lukáš
  • Špaček, Petr
  • Abart, Rainer
  • Ulrych, Jaromír
  • Habler, Gerlinde
http://linked.open...ain/vavai/riv/wos
  • 000322403300010
issn
  • 0022-3530
number of pages
http://bibframe.org/vocab/doi
  • 10.1093/petrology/egt028
http://localhost/t...ganizacniJednotka
  • 14310
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