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Late Paleozoic and Mesozoic evolution of the Lhasa Terrane in the Xainza area of southern Tibet 期刊论文
TECTONOPHYSICS, 2017, 卷号: 721, 期号: 0, 页码: 415-434
Authors:  Fan, SY (Fan, Suoya);  Ding, L (Ding, Lin);  Murphy, MA (Murphy, Michael A.);  Yao, W (Yao, Wei);  Yin, A (Yin, An);  Fan, SY
Adobe PDF(9424Kb)  |  Favorite  |  View/Download:894/1  |  Submit date:2018/05/16
Zircon U-pb  Bangong-nujiang Ocean  Indo-asian Collision  Retroarc Foreland Basin  Neo-tethys Ocean  Volcanic-rocks  Tectonic Implications  Northern Tibet  Suture Zone  Crustal Growth  
Tectonostratigraphy and provenance of an accretionary complex within the Yarlung-Zangpo suture zone, southern Tibet: Insights into subduction-accretion processes in the Neo-Tethys 期刊论文
TECTONOPHYSICS, 2012, 卷号: 574, 期号: 0, 页码: 181-192
Authors:  Cai FL (蔡福龙);  Ding L (丁林);  Leary RJ (Leary, Ryan J.);  Wang HQ (王厚起);  Xu Q (许强);  Zhang LY (张利云);  Yue YH (岳雅慧);  Cai, FL (通讯作者),Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China.
Adobe PDF(3654Kb)  |  Favorite  |  View/Download:1444/152  |  Submit date:2013/02/25
Zircon U-pb  Fore-arc Basin  Cenozoic Tectonic Evolution  Indo-asian Collision  Tsangpo Suture  Lhasa Terrane  Neotethyan Subduction  Gangdese Batholith  Cretaceous Strata  Xigaze Ophiolite  
Paleomagnetic evidence for clockwise rotation and tilting in the eastern Tethyan Himalaya (SE Tibet): Implications for the Miocene tectonic evolution of the NE Himalaya 期刊论文
TECTONOPHYSICS, 2010, 卷号: 493, 期号: 1-2, 页码: 172-186
Authors:  Antolin;  B (Antolin;  Borja);  Appel;  E (Appel;  Erwin);  Gloaguen;  R (Gloaguen;  Richard);  Dunkl;  I (Dunkl;  Istvan);  Ding L(丁林);  Montomoli;  C (Montomoli;  Chiara);  Liebke;  U (Liebke;  Ursina);  Xu Q(许强);  Antolin, B
Adobe PDF(4148Kb)  |  Favorite  |  View/Download:1467/184  |  Submit date:2011/04/07
INDIA-ASIA COLLISION  LEFT-SLIP FAULTS  SOUTHERN TIBET  CENTRAL NEPAL  OROGEN-PARALLEL  CONTINENTAL COLLISION  STRUCTURAL EVOLUTION  SOUTHEASTERN TIBET  WESTERN HIMALAYA  GROWTH-MECHANISM