中国科学院青藏高原研究所机构知识库
Advanced  
ITPCAS OpenIR  > 图书馆  > 期刊论文
学科主题: 地球科学::地球物理学
题名: Review of "orogenic plateau"
作者: Xu, ZQ (Xu ZhiQin)1, 2, 3, 4; Zhao, ZB (Zhao ZhongBao)2, 3; Peng, M (Peng Miao)4; Ma, XX (Ma XuXuan)2, 3; Li, HQ (Li HuaQi)2, 3; Zhao, JM (Zhao JunMeng)5
通讯作者: Xu, ZQ
关键词: CENTRAL ANDEAN PLATEAU ; EASTERN TIBETAN PLATEAU ; ALTIPLANO-PUNA PLATEAU ; SOUTHERN CENTRAL ANDES ; LATE MIOCENE RISE ; FOLD-THRUST BELT ; BOLIVIAN ANDES ; COLORADO PLATEAU ; COLLISION ZONE ; UNITED-STATES
刊名: ACTA PETROLOGICA SINICA
发表日期: 2016
卷: 32, 期:12, 页:3557-3571
收录类别: SCI
合作性质: 国内
文章类型: Review
英文摘要:  Plateaus on earth can be subdivided into two categories: craton plateau and orogenic plateau. Craton plateau normally developed on Precambrian basement or stable craton, which is characterized by simple, homogeneous, stable, cold and strong old basement, such as Brazilian Plateau, Colorado Plateau, Ethiopia Plateau, South African Plateau, Middle Siberia Plateau, Deccan Plateau, and so on. Basement of orogenic plateau is always composed by different orogenic units. The orogenic plateau could be separated into subducted orogenic plateau and collisional orogenic plateau two groups. The Middle Andean Plateau, formed overlying eastward subducted Pacific plate, belongs the subducted orogenic plateau. While, the Tibetan Plateau possess complex and uninformed soft basements which have experienced multiple phase orogeny. New research results illustrate that the Tibetan Plateau begin uplifted during Early Cretaceous, it may be related with closure of Bangong-Nujiang Ocean at 120 similar to 140Ma. However, India-Asian collision (60 similar to 50Ma) and concomitantly low angle under thrust of Indian lithosphere beneath Tibetan Plateau lead to the Plateau finally elevated over 4000 similar to 5000m.
语种: 英语
WOS记录号: WOS:000391345300001
Citation statistics:
内容类型: 期刊论文
URI标识: http://ir.itpcas.ac.cn/handle/131C11/7477
Appears in Collections:图书馆_期刊论文

Files in This Item:
File Name/ File Size Content Type Version Access License
V.32(12) 3557-3571 2016.pdf(5366KB)期刊论文作者接受稿开放获取View 联系获取全文

作者单位: 1.Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210046, Jiangsu, Peoples R China
2.CGS, Innovat Res Ctr Continental Tecton & Dynam, Beijing 100037, Peoples R China
3.CAGS, Inst Geol, Beijing 100037, Peoples R China
4.China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
5.Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100085, Peoples R China

Recommended Citation:
Xu, ZQ ,Zhao, ZB ,Peng, M ,et al. Review of "orogenic plateau"[J]. ACTA PETROLOGICA SINICA,2016,32(12):3557-3571.
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Xu, ZQ (Xu ZhiQin)]'s Articles
[Zhao, ZB (Zhao ZhongBao)]'s Articles
[Peng, M (Peng Miao)]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Xu, ZQ (Xu ZhiQin)]‘s Articles
[Zhao, ZB (Zhao ZhongBao)]‘s Articles
[Peng, M (Peng Miao)]‘s Articles
Related Copyright Policies
Null
Social Bookmarking
Add to CiteULike Add to Connotea Add to Del.icio.us Add to Digg Add to Reddit
文件名: V.32(12) 3557-3571 2016.pdf
格式: Adobe PDF
所有评论 (0)
暂无评论
 
评注功能仅针对注册用户开放,请您登录
您对该条目有什么异议,请填写以下表单,管理员会尽快联系您。
内 容:
Email:  *
单位:
验证码:   刷新
您在IR的使用过程中有什么好的想法或者建议可以反馈给我们。
标 题:
 *
内 容:
Email:  *
验证码:   刷新

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.

 

 

Valid XHTML 1.0!
Copyright © 2007-2018  中国科学院青藏高原研究所 - Feedback
Powered by CSpace