About: Clasts of Variscan high-grade rocks within Upper Visean conglomerates - a missing link in the late Variscan evolution of Central Europe: constraints from U-Pb chronology     Goto   Sponge   NotDistinct   Permalink

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  • In this paper, U-Pb zircon, monazite and rutile data for crystalline rocks deposited as clasts in the Upper Visean conglomerates at the eastern margin of the Bohemian Massif are reported. U-Pb data of spherical zircon from three different granulite clasts yielded a mean age of 339.0 +- 0.7 Ma, while oval and spherical grains of another granulite pebble define a slightly younger date of 337.1 +- 1.1 Ma. These ages are interpreted as dating granulite facies metamorphism. Thermochronology and the derived pressure–temperature (P–T) path of the granulite pebbles reflect two-stage exhumation of the granulites. Near-to-isothermal decompression from at least 44 km to mid-crustal depths of around 22 km was followed by a near-isobaric cooling stage based on reaction textures and geothermobarometry. Minimum average exhumation rate corresponds to 2.8–4.3 mm/year. The extensive medium-pressure/ high-temperature overprint on granulite assemblages is dated by U-Pb in monazite at c. 333 Ma.
  • In this paper, U-Pb zircon, monazite and rutile data for crystalline rocks deposited as clasts in the Upper Visean conglomerates at the eastern margin of the Bohemian Massif are reported. U-Pb data of spherical zircon from three different granulite clasts yielded a mean age of 339.0 +- 0.7 Ma, while oval and spherical grains of another granulite pebble define a slightly younger date of 337.1 +- 1.1 Ma. These ages are interpreted as dating granulite facies metamorphism. Thermochronology and the derived pressure–temperature (P–T) path of the granulite pebbles reflect two-stage exhumation of the granulites. Near-to-isothermal decompression from at least 44 km to mid-crustal depths of around 22 km was followed by a near-isobaric cooling stage based on reaction textures and geothermobarometry. Minimum average exhumation rate corresponds to 2.8–4.3 mm/year. The extensive medium-pressure/ high-temperature overprint on granulite assemblages is dated by U-Pb in monazite at c. 333 Ma. (en)
Title
  • Clasts of Variscan high-grade rocks within Upper Visean conglomerates - a missing link in the late Variscan evolution of Central Europe: constraints from U-Pb chronology
  • Clasts of Variscan high-grade rocks within Upper Visean conglomerates - a missing link in the late Variscan evolution of Central Europe: constraints from U-Pb chronology (en)
skos:prefLabel
  • Clasts of Variscan high-grade rocks within Upper Visean conglomerates - a missing link in the late Variscan evolution of Central Europe: constraints from U-Pb chronology
  • Clasts of Variscan high-grade rocks within Upper Visean conglomerates - a missing link in the late Variscan evolution of Central Europe: constraints from U-Pb chronology (en)
skos:notation
  • RIV/00216224:14310/07:00020843!RIV10-MSM-14310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/99/0567), Z(MSM0021622412)
http://linked.open...iv/cisloPeriodika
  • 8
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
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  • 413878
http://linked.open...ai/riv/idVysledku
  • RIV/00216224:14310/07:00020843
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • clast Upper Visean conglomerates U/Pb geochronology (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • GB - Spojené království Velké Británie a Severního Irska
http://linked.open...ontrolniKodProRIV
  • [543FDDD3ADC6]
http://linked.open...i/riv/nazevZdroje
  • Journal of metamorphic Geology
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
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http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 25
http://linked.open...iv/tvurceVysledku
  • Novák, Milan
  • Kotková, Jana
  • Gerdes, Axel
  • Parrish, R. R.
http://linked.open...n/vavai/riv/zamer
issn
  • 0263-4929
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  • 14310
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