北吕宋岛菲律宾活动带蛇绿岩及其上覆浊积岩的放射虫研究新进展
    点此下载全文
引用本文:Keisuke ISHIDA,Shigeyuki SUZUKI,Carla DIMALANTA,Graciano YUMUL JR.,Karlo QUEAÑO,Decibel FAUSTINO-ESLAVA,Edanjarlo MARQUEZ,Noelynna RAMOS,Rolando PEÑA.2012.北吕宋岛菲律宾活动带蛇绿岩及其上覆浊积岩的放射虫研究新进展[J].地球学报,33(s1):29-31.
DOI:10.3975/cagsb.2012.s1.15
摘要点击次数: 2456
全文下载次数: 5116
作者单位E-mail
Keisuke ISHIDA Institute of Socio-Arts and Sciences, University of Tokushima ishidak@ias.tokushima-u.ac.jp 
Shigeyuki SUZUKI Department of Earth Sciences, Okayama University  
Carla DIMALANTA Rushurgent Working Group, National Institute of Geological Sciences, University of the Philippines  
Graciano YUMUL JR. Monte Oro Resources and Energy Inc.  
Karlo QUEAÑO Mines and Geosciences Bureau  
Decibel FAUSTINO-ESLAVA School of Environmental Science and Management, University of the Philippines – Los Ba?os  
Edanjarlo MARQUEZ Department of Physical Sciences and Mathematics, University of the Philippines – Manila  
Noelynna RAMOS Rushurgent Working Group, National Institute of Geological Sciences, University of the Philippines  
Rolando PEÑA Mines and Geosciences Bureau (MGB)  
中文摘要:The basement of the Philippine Mobile Belt (PMB) is mainly composed of ophiolites that are mostly overlain by Paleogene to Miocene turbidites in central Luzon. To clarify the geological development of the PMB with respect to the initial stage of the arc volcanism (eg. Yumul et al., 2003, 2008; Dimalanta and Yumul, 2003; Suzuki et al., 2011), radiolarian dating was examined in siliceous sediments associated with the ophiolites and turbidites. The samples were collected from sites identified with the Zambales and Montalban ophiolites, basic tuff phyllites in NW Din-galan, and their overlying formations.
中文关键词:Philippine Mobile Belt  Radiolarian fauna  Ophiolitic Complex  Turbidites
 
Recent Progress in Radiolarian Research for Ophiolites and the Overlying Turbidites, Philippine Mobile Belt, Northern Luzon Island
Abstract:The basement of the Philippine Mobile Belt (PMB) is mainly composed of ophiolites that are mostly overlain by Paleogene to Miocene turbidites in central Luzon. To clarify the geological development of the PMB with respect to the initial stage of the arc volcanism (eg. Yumul et al., 2003, 2008; Dimalanta and Yumul, 2003; Suzuki et al., 2011), radiolarian dating was examined in siliceous sediments associated with the ophiolites and turbidites. The samples were collected from sites identified with the Zambales and Montalban ophiolites, basic tuff phyllites in NW Din-galan, and their overlying formations.
keywords:Philippine Mobile Belt  Radiolarian fauna  Ophiolitic Complex  Turbidites
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:中华人民共和国自然资源部 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:北京勤云科技发展有限公司
京ICP备05029128号-6

京公网安备 11010202007616号