About: Rate of erosion and exhumation of crystalline rocks in the Hunza Karakoram defined by apatite fission track analysis     Goto   Sponge   NotDistinct   Permalink

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  • Rapid exhumation of rock massifs in the Hunza Karakoram has been caused by collision orogeny as well as intensive and variable climate-morphogenetic processes during the late Cenozoic. Apatite fission-track dating of crystalline rocks gave AFT-ages between 3.9 +/- 0.2 Ma to 9.9 +/- 0.4 Ma and constrained the period of a rapid exhumation and unroofing as Upper Miocene to Quaternary. Time-temperature curves of the samples show two trends of exhumation rate: the Upper Miocene to Pliocene period of a slow rate of ca. 0.1 km/Ma followed by the Quaternary period of a relative rapid rate of ca. 2.6 km/Ma. The erosion rate reached up to a maximum of ca. 4000 m from the Upper Miocene to the present. The high intensity of recent denudation and transport of weathered and eroded material suggest their long-term influence on the exhumation of deeper parts of the rock massifs during active orogenetic processes in the Hunza Karakoram.
  • Rapid exhumation of rock massifs in the Hunza Karakoram has been caused by collision orogeny as well as intensive and variable climate-morphogenetic processes during the late Cenozoic. Apatite fission-track dating of crystalline rocks gave AFT-ages between 3.9 +/- 0.2 Ma to 9.9 +/- 0.4 Ma and constrained the period of a rapid exhumation and unroofing as Upper Miocene to Quaternary. Time-temperature curves of the samples show two trends of exhumation rate: the Upper Miocene to Pliocene period of a slow rate of ca. 0.1 km/Ma followed by the Quaternary period of a relative rapid rate of ca. 2.6 km/Ma. The erosion rate reached up to a maximum of ca. 4000 m from the Upper Miocene to the present. The high intensity of recent denudation and transport of weathered and eroded material suggest their long-term influence on the exhumation of deeper parts of the rock massifs during active orogenetic processes in the Hunza Karakoram. (en)
Title
  • Rate of erosion and exhumation of crystalline rocks in the Hunza Karakoram defined by apatite fission track analysis
  • Rate of erosion and exhumation of crystalline rocks in the Hunza Karakoram defined by apatite fission track analysis (en)
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  • Rate of erosion and exhumation of crystalline rocks in the Hunza Karakoram defined by apatite fission track analysis
  • Rate of erosion and exhumation of crystalline rocks in the Hunza Karakoram defined by apatite fission track analysis (en)
skos:notation
  • RIV/00216208:11310/14:10282184!RIV15-MSM-11310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, Z(AV0Z30130516)
http://linked.open...iv/cisloPeriodika
  • 3
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
  • 41388
http://linked.open...ai/riv/idVysledku
  • RIV/00216208:11310/14:10282184
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • history; collision; geochronology; thermochronology; Ladakh; Himalaya; Northern Pakistan; transantarctic mountains; suture zone; Karakoram; erosion; exhumation of rocks; apatite fission track analysis (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [AE18668BC7E6]
http://linked.open...i/riv/nazevZdroje
  • Acta Geodynamica et Geomaterialia
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 11
http://linked.open...iv/tvurceVysledku
  • Svojtka, Martin
  • Kalvoda, Jan
  • Korinkova, Dagmar
http://linked.open...ain/vavai/riv/wos
  • 000339385500005
http://linked.open...n/vavai/riv/zamer
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  • 1214-9705
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  • 11310
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