ORCID Profile
0000-0003-2639-3212
Current Organisations
Trinity College Dublin
,
Chinese Academy of Geological Sciences Institute of Geology
,
Syracuse University
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Publisher: American Geophysical Union (AGU)
Date: 03-2017
DOI: 10.1002/2017JB014006
Publisher: Elsevier BV
Date: 11-2013
Publisher: Wiley
Date: 10-2016
Publisher: Elsevier BV
Date: 03-2012
Publisher: Elsevier BV
Date: 10-2013
Publisher: Elsevier BV
Date: 2016
Publisher: Geological Society of America
Date: 17-10-2017
DOI: 10.1130/B31771.1
Publisher: Elsevier BV
Date: 10-2013
Publisher: Springer Science and Business Media LLC
Date: 11-05-2016
DOI: 10.1038/SREP25751
Abstract: A compilation of U-Pb age, geochemical and isotopic data for granitoid plutons in the southern Central Asian Orogenic Belt (CAOB), enables evaluation of the interaction between magmatism and orogenesis in the context of Paleo-Asian oceanic closure and continental amalgamation. These constraints, in conjunction with other geological evidence, indicate that following consumption of the ocean, collision-related calc-alkaline granitoid and mafic magmatism occurred from 255 ± 2 Ma to 251 ± 2 Ma along the Solonker-Xar Moron suture zone. The linear or belt distribution of end-Permian magmatism is interpreted to have taken place in a setting of final orogenic contraction and weak crustal thickening, probably as a result of slab break-off. Crustal anatexis slightly post-dated the early phase of collision, producing adakite-like granitoids with some S-type granites during the Early-Middle Triassic (ca. 251–245 Ma). Between 235 and 220 Ma, the local tectonic regime switched from compression to extension, most likely caused by regional lithospheric extension and orogenic collapse. Collision-related magmatism from the southern CAOB is thus a prime ex le of the minor, yet tell-tale linking of magmatism with orogenic contraction and collision in an archipelago-type accretionary orogen.
Publisher: American Geophysical Union (AGU)
Date: 06-2014
DOI: 10.1002/2013TC003444
Publisher: American Geophysical Union (AGU)
Date: 04-2017
DOI: 10.1002/2016TC004422
Location: China
No related grants have been discovered for Shan Li.