Developing the plate tectonics from oceanic subduction to continental collision
Zheng YongFei1; Ye Kai2; Zhang LiFei3
刊名CHINESE SCIENCE BULLETIN
2009-08-01
卷号54期号:15页码:2549-2555
关键词crustal subduction continental collision ultrahigh-pressure metamorphism continental dynamics
ISSN号1001-6538
DOI10.1007/s11434-009-0464-0
文献子类Article
英文摘要The studies of continental deep subduction and ultrahigh-pressure metamorphism have not only promoted the development of solid earth science in China, but also provided an excellent opportunity to advance the plate tectonics theory. In view of the nature of subducted crust, two types of subduction and collision have been respectively recognized in nature. On one hand, the crustal subduction occurs due to underflow of either oceanic crust (Pacific type) or continental crust (Alpine type). On the other hand, the continental collision proceeds by arc-continent collision (Himalaya-Tibet type) or continent-continent collision (Dabie-Sulu type). The key issues in the future study of continental dynamics are the chemical changes and differential exhumation in continental deep subduction zones, and the temporal-spatial transition from oceanic subduction to continental subduction.
WOS关键词PRESSURE METAMORPHIC ROCKS ; SULU OROGENIC BELT ; DABIE OROGEN ; ISOTOPE GEOCHEMISTRY ; EASTERN CHINA ; ZIRCON GROWTH ; FLUID REGIME ; UHP TERRANE ; U-PB ; CRUST
WOS研究方向Science & Technology - Other Topics
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:000268571300001
资助机构Chinese Academy of Sciences(kzcx2-yw-131) ; Chinese Academy of Sciences(kzcx2-yw-131) ; Ministry of Science and Technology of China(2009CB825000) ; Ministry of Science and Technology of China(2009CB825000) ; Chinese Academy of Sciences(kzcx2-yw-131) ; Chinese Academy of Sciences(kzcx2-yw-131) ; Ministry of Science and Technology of China(2009CB825000) ; Ministry of Science and Technology of China(2009CB825000) ; Chinese Academy of Sciences(kzcx2-yw-131) ; Chinese Academy of Sciences(kzcx2-yw-131) ; Ministry of Science and Technology of China(2009CB825000) ; Ministry of Science and Technology of China(2009CB825000) ; Chinese Academy of Sciences(kzcx2-yw-131) ; Chinese Academy of Sciences(kzcx2-yw-131) ; Ministry of Science and Technology of China(2009CB825000) ; Ministry of Science and Technology of China(2009CB825000)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/71308]  
专题中国科学院地质与地球物理研究所
通讯作者Zheng YongFei
作者单位1.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Peking Univ, Sch Earth & Space Sci, MOE Key Lab Orogen Belt & Crustal Evolut, Beijing 100871, Peoples R China
推荐引用方式
GB/T 7714
Zheng YongFei,Ye Kai,Zhang LiFei. Developing the plate tectonics from oceanic subduction to continental collision[J]. CHINESE SCIENCE BULLETIN,2009,54(15):2549-2555.
APA Zheng YongFei,Ye Kai,&Zhang LiFei.(2009).Developing the plate tectonics from oceanic subduction to continental collision.CHINESE SCIENCE BULLETIN,54(15),2549-2555.
MLA Zheng YongFei,et al."Developing the plate tectonics from oceanic subduction to continental collision".CHINESE SCIENCE BULLETIN 54.15(2009):2549-2555.
个性服务
查看访问统计
相关权益政策
暂无数据
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。


©版权所有 ©2017 CSpace - Powered by CSpace