ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
伊朗南部高扎格罗斯浊积放射虫岩亚带的放射虫地层学
  
关键词:Zagros  southern Iran  radiolarite  Cretaceous  Jurassic
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作者单位E-mail
Ken-ichiro HISADA Graduate School of Life and Environmental Sciences, University of Tsukuba hisadak@geol.tsukuba.ac.jp 
Yoshihito KAMATA Graduate School of Life and Environmental Sciences, University of Tsukuba  
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摘要:
Stratigraphy of Radiolarite in the Turbiditic Radiolaritic Subzone of the High Zagros, Southern Iran
      Zagros orogen extends from the Turkish-Iranian border to NW, to the Makran area in SE. According to Geological Survey of Iran 100,000 series “Sureyan”, “Saadatshahr”, “Abadeh-E-Tashk” and “Arsenjan”, the Zagros orogen comprises the following sub-parallel tectonostratigraphic domains, from SW to NE: the Zagros foreland basin, the Simply Foloded Belt, the more mountainous part of the Zagros proper (includ-ing the High Zagros and the Crush Zone) and domains that can be thought of belonging to the Zagros orogen in a broader sense: the SSZ (Sanadaj-Sirijan Zone), the UDMA (Urumiyeh-Dokhtar Magmatic Arc) and the western parts of Central Iran.
Ken-ichiro HISADA,Yoshihito KAMATA.2012.Stratigraphy of Radiolarite in the Turbiditic Radiolaritic Subzone of the High Zagros, Southern Iran[J].Acta Geoscientica Sinica,33(s1):18-20.
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