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Statements

Subject Item
dbr:High_pressure_metamorphic_terranes_along_the_Bangong-Nujiang_Suture_Zone
rdfs:label
High pressure metamorphic terranes along the Bangong-Nujiang Suture Zone
rdfs:comment
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.
foaf:depiction
n12:Ofiolite_sequence_EN.svg n12:Cross_section_depicting_the_tectonic_evolution_of_the_Bangong_suture_zone.png n12:Bangong-Nujiang_Suture_Zone.png n12:Metamorphic_Facies_Diagram.png
dcterms:subject
dbc:Prehistoric_Tibet dbc:Upper_Jurassic_Series dbc:Lower_Cretaceous_Series_of_Asia dbc:Jurassic_Asia dbc:Geology_of_Tibet
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40482685
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1054546657
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dbr:Microcontinent dbr:Late_Jurassic dbr:Subduction_zone dbr:Amphibolite dbr:Metasediment dbr:Mesozoic dbr:Transhimalaya dbr:Mélange dbr:Harzburgite dbr:Sinistral_fault dbr:Diorite dbr:Gabbro dbr:Upper_mantle_(Earth) dbr:Obduction dbr:Orogenic dbr:Viscous dbr:Tonalite dbc:Upper_Jurassic_Series dbr:Amdo,_Tibet dbc:Prehistoric_Tibet dbr:Continental_lithosphere dbr:Lhasa_terrane dbr:Serpentinites dbr:Triassic dbr:Eduction_(geology) dbr:Kbar dbr:Tethys_Ocean dbr:Terrane dbr:Geology_of_the_Himalaya dbr:Tibetan_Plateau dbr:Bangong_Lake dbr:Crustal_thickening dbc:Lower_Cretaceous_Series_of_Asia dbr:Nujiang,_Tibet dbr:Middle_Jurassic dbr:Marble dbr:Orthogneiss dbr:Ductile dbr:Indus-Yarlung_suture_zone dbr:Volcaniclastic dbr:Ultra-high-pressure_metamorphism dbr:Bangong_suture dbr:Granodiorite dbr:Peridotite dbr:Chert dbr:Shear_(geology) dbr:Quartzite dbr:MORB dbr:Dongqiao,_Tibet dbr:Paragneiss dbr:Gabbros n18:Cross_section_depicting_the_tectonic_evolution_of_the_Bangong_suture_zone.png n18:Ofiolite_sequence_EN.svg dbr:Serpentine_group dbr:Sheeted_dyke_complex dbr:Dingqing dbr:Ultramafic dbr:Slab_detachment dbc:Jurassic_Asia dbr:Qiangtang_terrane dbr:Samarium–neodymium_dating dbr:Thrust_fault dbr:P-T dbr:Diachronous dbr:Jurassic dbr:Eclogites dbr:Early_Cretaceous dbr:SHRIMP dbr:Subduction dbr:Permian-Triassic dbr:Ophiolites dbr:Pelagic dbr:Pillow_basalts dbr:Suture_(geology) dbr:Slab_rollback dbr:Massif dbr:Serpentinite dbr:Schist n18:Bangong-Nujiang_Suture_Zone.png dbr:Ocean_basin dbc:Geology_of_Tibet dbr:Back-arc dbr:Zircons n18:Metamorphic_Facies_Diagram.png
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dbt:Reflist dbt:Course_assignment dbt:Short_description
dbo:thumbnail
n12:Bangong-Nujiang_Suture_Zone.png?width=300
dbp:course
Education Program:Louisiana State University/GEOL 4066: Plate Tectonics
dbp:term
2013
dbo:abstract
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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