High pressure terranes along the ~1200 km long east-west trending Bangong-Nujiang suture zone (BNS) on the Tibetan Plateau have been extensively mapped and studied. Understanding the geodynamic processes in which these terranes are created is key to understanding the development and subsequent deformation of the BNS and Eurasian deformation as a whole.

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  • High pressure metamorphic terranes along the Bangong-Nujiang Suture Zone (en)
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  • High pressure terranes along the ~1200 km long east-west trending Bangong-Nujiang suture zone (BNS) on the Tibetan Plateau have been extensively mapped and studied. Understanding the geodynamic processes in which these terranes are created is key to understanding the development and subsequent deformation of the BNS and Eurasian deformation as a whole. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Ofiolite_sequence_EN.svg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Bangong-Nujiang_Suture_Zone.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Cross_section_depicting_the_tectonic_evolution_of_the_Bangong_suture_zone.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Metamorphic_Facies_Diagram.png
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