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中国科学院海洋研究所机构知识库
Knowledge Management System Of Institute of Oceanology, Chinese Academy of Sciences
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Tracing the subduction and accretion history of the trench-arc-basin system in the Chinese Eastern Tianshan: Insights from Paleozoic magmatic and crustal evolution
期刊论文
EARTH-SCIENCE REVIEWS, 2024, 卷号: 252, 页码: 21
作者:
Du, Long
;
Long, Xiaoping
;
Yuan, Chao
;
Zhang, Yunying
;
Huang, Zongying
;
Zhu, Hongli
收藏
  |  
浏览/下载:9/0
  |  
提交时间:2024/08/29
Central Asian Orogenic Belt (CAOB)
Eastern Tianshan
Kangguer Ocean
Igneous rocks
Crustal evolution
Multi-scale ocean dynamical processes in the Indo-Pacific Convergence Zone and their climatic and ecological effects
期刊论文
EARTH-SCIENCE REVIEWS, 2023, 卷号: 237, 页码: 25
作者:
Du, Yan
;
Wang, Fan
;
Wang, Tianyu
;
Liu, Weiwei
;
Liang, Linlin
;
Zhang, Ying
;
Chen, Yunfan
;
Liu, Jiaxing
;
Wu, Wei
;
Yu, Kefu
;
Zhang, Jing
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  |  
浏览/下载:235/0
  |  
提交时间:2023/12/13
Indo-Pacific Convergence Zone
Ocean dynamical processes
Ocean circulation
Marine ecological effects
Climate change
Porphyry copper and skarn fertility of the northern Qinghai-Tibet Plateau collisional granitoids
期刊论文
EARTH-SCIENCE REVIEWS, 2021, 卷号: 214, 页码: 22
作者:
Zhong, Shihua
;
Li, Sanzhong
;
Feng, Chengyou
;
Liu, Yongjiang
;
Santosh, M.
;
He, Shuyue
;
Qu, Hongying
;
Liu, Guoyan
;
Seltmann, Reimar
;
Lai, Zhiqing
;
Wang, Xiaohong
;
Song, Yingxin
;
Zhou, Jie
Adobe PDF(26503Kb)
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浏览/下载:408/0
  |  
提交时间:2021/04/21
Collisional tectonics
Flat slab subduction
Porphyry copper deposits
Skarn deposits
Qinghai-Tibet Plateau (QTP)
The petrological control on the lithosphere-asthenosphere boundary (LAB) beneath ocean basins
期刊论文
EARTH-SCIENCE REVIEWS, 2018, 卷号: 185, 页码: 301-307
作者:
Niu, Yaoling
;
Green, David H.
Adobe PDF(2410Kb)
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浏览/下载:201/0
  |  
提交时间:2019/05/15
Lithosphere-asthenosphere boundary
LAB
Petrological control
Amphibole dehydration solidus
Petrology-controlled sub-LAB convection
Plate model
Juxtaposed sequence stratigraphy, temporal-spatial variations of sedimentation and development of modern-forming forearc Lichi Melange in North Luzon Trough forearc basin onshore and offshore eastern Taiwan: An overview
期刊论文
EARTH-SCIENCE REVIEWS, 2018, 卷号: 182, 页码: 102-140
作者:
Huang, Chi-Yue
;
Chen, Wen-Huang
;
Wang, Ming-Huei
;
Lin, Chiou-Ting
;
Yang, Shengxiong
;
Li, Xuejie
;
Yu, Mengming
;
Zhao, XiXi
;
Yang, Kenn-Ming
;
Liu, Char-Shine
;
Hsieh, Yu-Huan
;
Harris, Ron
Adobe PDF(20748Kb)
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浏览/下载:459/0
  |  
提交时间:2019/08/21
Juxtaposed forearc sequences
Bivergent thrusting
syn-Sedimentation deformation
Oblique collision
Lichi Melange
Reconstructing chemical weathering, physical erosion and monsoon intensity since 25 Ma in the northern South China Sea: A review of competing proxies
期刊论文
EARTH-SCIENCE REVIEWS, 2014, 卷号: 130, 页码: 86-102
作者:
Clift, Peter D.
;
Wan, Shiming
;
Blusztajn, Jerzy
;
Clift, PD (reprint author), Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA.
Adobe PDF(3751Kb)
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浏览/下载:289/0
  |  
提交时间:2015/06/11
Monsoon
Erosion
Weathering
Clay Mineralogy
Sediment Geochemistry
South China Sea
Continental orogenesis from ocean subduction, continent collision/subduction, to orogen collapse, and orogen recycling: The example of the North Qaidam UHPM belt, NW China
期刊论文
EARTH-SCIENCE REVIEWS, 2014, 卷号: 129, 页码: 59-84
作者:
Song, Shuguang
;
Niu, Yaoling
;
Su, Li
;
Zhang, Cong
;
Zhang, Lifei
;
Song, SG (reprint author), Peking Univ, Sch Earth & Space Sci, MOE Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China.
Adobe PDF(8586Kb)
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浏览/下载:283/0
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提交时间:2015/06/11
Continental-type Uhpm Belt
Post-collisional Magmatism
Orogenesis And Mountain Collapse
Decoupling Of Oceanic And Continental
Subduction Belts
Orogen Recycling
Northern Tibetan Plateau
Continental collision zones are primary sites for net continental crust growth - A testable hypothesis
期刊论文
EARTH-SCIENCE REVIEWS, 2013, 卷号: 127, 页码: 96-110
作者:
Niu, Yaoling
;
Zhao, Zhidan
;
Zhu, Di-Cheng
;
Mo, Xuanxue
;
Niu, YL
Adobe PDF(3421Kb)
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浏览/下载:294/0
  |  
提交时间:2014/07/17
Continental Collision
Ocean Crust Melting
Syncollisional Granitoid Magmatism
Juvenile Crust Formation
Episodic Continental Crust Growth
Super-continental Amalgamation
Daly Gap