ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
伊朗中部原特提斯残余的评价及构造环境:据地球化学研究
  
关键词:Gneisses  ultra-mafic rocks  Central Iran  Saghand  Posht-e-Badam
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Monireh POSHTKOOHI Geological Survey of Iran m_poshtkoohi@yahoo.com 
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摘要:
Evaluation of Tectonic Setting of the Proto-tethyan Remnants in Central Iran: A Geochemical Study
      The Iranian plateau comprises several continental blocks, which are clearly bounded by major faults. The sedimentary, stratigraphic, magmatic and metamorphic features of these blocks vary from one to the other. The continental crust of subject area in Central Iran was investigated in the past by several authors. It was concluded that this zone was metamorphosed, intruded by granites and faulted during late Precambrian Pan-African Orogeny (Ramezani and Tucker, 2003).
Monireh POSHTKOOHI.2012.Evaluation of Tectonic Setting of the Proto-tethyan Remnants in Central Iran: A Geochemical Study[J].Acta Geoscientica Sinica,33(s1):55-57.
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