Neogene exhumation of the Marrakech High Atlas (Morocco) recorded by apatite fission-track analysis. (Articolo in rivista)

Type
Label
  • Neogene exhumation of the Marrakech High Atlas (Morocco) recorded by apatite fission-track analysis. (Articolo in rivista) (literal)
Anno
  • 2009-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1111/j.1365-3121.2008.00857.x (literal)
Alternative label
  • Balestrieri M.; Moratti G.; Bigazzi G.; Algouti A. (2009)
    Neogene exhumation of the Marrakech High Atlas (Morocco) recorded by apatite fission-track analysis.
    in TERRA nova (Print)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Balestrieri M.; Moratti G.; Bigazzi G.; Algouti A. (literal)
Pagina inizio
  • 75 (literal)
Pagina fine
  • 82 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 21 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
  • In: Terra Nova, vol. 21 (2) pp. 75 - 82. Blackwell, 2009. (literal)
Note
  • ISI Web of Science (WOS) (literal)
  • Scopu (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • CNR, Istituto di Geoscienze e Georisorse, Via La Pira 4, 50121 Firenze, Italy; CNR, Istituto di Geoscienze e Georisorse, Via Moruzzi 1, 56124 Pisa, Italy; Universite´ Cadi Ayyad, Faculte´ des Sciences Semlalia, BP S ? 15, Marrakech, Morocco (literal)
Titolo
  • Neogene exhumation of the Marrakech High Atlas (Morocco) recorded by apatite fission-track analysis. (literal)
Abstract
  • Apatite fission-track (AFT) data have been obtained along a traverse across the Marrakech High Atlas to constrain its tectono-thermal evolution. AFT ages vary between 212 ± 15 Ma and 20 ± 4 Ma. An Early Miocene AFT age accompanied by long mean track length from the central part of the chain has been interpreted as the timing of the main inversion of this region with the creation of relief because of the shortening induced by the interplay between the African and Eurasian plates. Thermal modelling of samples collected south of the South Atlas Fault Zone indicates a Middle-Late Miocene or even later cooling that has been attributed to the component of the uplift of the chain related to the thermal anomaly present beneath the Atlas Mountains. (literal)
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