Late Mesozoic crustal extension along the southern Eurasian margin: evidence from volcanic rocks of the Bangong-Nujiang Suture zone, Tibet
    点此下载全文
引用本文: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 Eurasian margin: evidence from volcanic rocks of the Bangong-Nujiang Suture zone, Tibet[J].地球学报,30(S1):8.
DOI:10.3975/cagsb.2009.s1.05
摘要点击次数: 15951
全文下载次数: 1891
作者单位E-mail
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  
中文摘要: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).
 
Late Mesozoic crustal extension along the southern Eurasianmargin: evidence from volcanic rocks of the Bangong-NujiangSuture zone, Tibet
Abstract: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).
查看全文  查看/发表评论  下载PDF阅读器
版权所有 《地球学报》编辑部 Copyright©2008 All Rights Reserved
主管单位:国土资源部 主办单位:中国地质科学院
地址: 北京市西城区百万庄大街26号,中国地质科学院东楼317室 邮编:100037 电话:010-68327396 E-mail: diqiuxb@126.com
技术支持:东方网景