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Late Mesozoic crustal extension along the southern Eurasian margin: evidence from volcanic rocks of the Bangong-Nujiang Suture zone, Tibet
  
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Decibel FAUSTINO-ESLAVA Rushurgent Working Group, Tectonics and Geodynamics Laboratory, National Institute of Geological Sciences, College of Science, University of the Philippines, Diliman 1101, Quezon City, Philippines decibel@graduate.hku.hk 
Jonathan A. AITCHISON Department or Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong  
Rodolfo A. TAMAYO Rushurgent Working Group, Tectonics and Geodynamics Laboratory, National Institute of Geological Sciences, College of Science, University of the Philippines, Diliman 1101, Quezon City, Philippines  
Jr.Graciano P. YUMUL Rushurgent Working Group, Tectonics and Geodynamics Laboratory, National Institute of Geological Sciences, College of Science, University of the Philippines, Diliman 1101, Quezon City, Philippines Office of the Undersecretary for Research and Development,  
Jr.Carla B. DIMALANTA Rushurgent Working Group, Tectonics and Geodynamics Laboratory, National Institute of Geological Sciences, College of Science, University of the Philippines, Diliman 1101, Quezon City, Philippines  
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Late Mesozoic crustal extension along the southern Eurasianmargin: evidence from volcanic rocks of the Bangong-NujiangSuture zone, Tibet
      The Mesozoic was a period of marginal basin formations, closures and reactivations along segments of the southern Eurasian margin. Remnants of some of these events are now preserved as exposures of Juras-sic-Cretaceous ophiolites and ophiolitic mélanges, thick sequences of Jurassic flysch deposits and Middle Cretaceous sedimentary and volcanic formations along the Bangong-Nujiang Suture Zone (BNS).
Decibel FAUSTINO-ESLAVA,Jonathan A. AITCHISON,Rodolfo A. TAMAYO,Jr.Graciano P. YUMUL,Jr.Carla B. DIMALANTA.2009.Late Mesozoic crustal extension along the southern Eurasianmargin: evidence from volcanic rocks of the Bangong-NujiangSuture zone, Tibet[J].Acta Geoscientica Sinica,30(S1):8.
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