K-Ar biotite ages from Miocene post-collisional Garam Chashma leucogranite, eastern Hindukush Range (Trans-Himalayas), northwestern Pakistan.

DOI 2 Citations 41 References Open Access
  • ZAFAR Mohammad
    Department of Geosciences, Faculty of Science, Naruto University of Education
  • MURATA Mamoru
    Department of Geosciences, Faculty of Science, Naruto University of Education
  • KHAN Tahseenullah
    Geoscience Laboratory, Geological Survey of Pakistan
  • OZAWA Hiroaki
    Department of Geosciences, Faculty of Science, Naruto University of Education
  • NISHIMURA Hiroshi
    Department of Geosciences, Faculty of Science, Naruto University of Education

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Description

Garam Chashma granitic rocks intrude discordantly into the Hindukush metamorphic complex on the southern margin of the Asian plate, Trans-Himalayas, northwestern Pakistan. The rocks are fine to coarse-grained, two-mica leucogranite. K-Ar biotite analyses of four samples from the Garam Chashma pluton yield 18-20 Ma ages. These ages are younger than those of the other post-collisional granitic rocks in Trans-Himalayas of Pakistan and resemble those of the Higher Himalayan granitic rocks.

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Details 詳細情報について

  • CRID
    1390001206544694528
  • NII Article ID
    10004952066
  • NII Book ID
    AA11460926
  • DOI
    10.2465/jmps.95.101
  • ISSN
    13493825
    13456296
    http://id.crossref.org/issn/13456296
  • Text Lang
    en
  • Data Source
    • JaLC
    • Crossref
    • CiNii Articles
    • OpenAIRE
  • Abstract License Flag
    Disallowed

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