Ordovician-Devonian multiple-phase subduction-accretion with crust-mantle interactions in the Proto-Tethys: Implications for plate driving mechanism
Miao Sang(Chinese Academy of Sciences), Luyao Wang(University of Oxford), Jingmin Gan(Chinese Academy of Sciences), Yunyan Ni(China University of Petroleum, Beijing), Yang He(Chinese Academy of Sciences), Wenjiao Xiao(Chinese Academy of Sciences), Xiaoliang Jia(Chinese Academy of Sciences), Zhou Tan(Chinese Academy of Sciences), Zhen Yan(Chinese Academy of Geological Sciences)
Cited by 0
Related Papers
Tectonic models for accretion of the Central Asian Orogenic Belt
|Journal of the Geological Society|2006|3.4k
Early Paleozoic to Devonian multiple-accretionary model for the Qilian Shan, NW China
|Journal of Asian Earth Sciences|2008|430
Geochemical, Sr–Nd and zircon U–Pb–Hf isotopic studies of Late Carboniferous magmatism in the West Junggar, Xinjiang: Implications for ridge subduction?
|Chemical Geology|2009|388
Zircon U–Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic
|Chemical Geology|2007|345
Archean crustal evolution of the northern Tarim craton, NW China: Zircon U–Pb and Hf isotopic constraints
|Precambrian Research|2010|325