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Sun, Weidong, Li, Shuguang, Chen, Yadong, Li, Yujing (2002) Timing of Synorogenic Granitoids in the South Qinling, Central China: Constraints on the Evolution of the Qinling‐Dabie Orogenic Belt. The Journal of Geology, 110 (4) 457-468 doi:10.1086/340632

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Reference TypeJournal (article/letter/editorial)
TitleTiming of Synorogenic Granitoids in the South Qinling, Central China: Constraints on the Evolution of the Qinling‐Dabie Orogenic Belt
JournalThe Journal of Geology
AuthorsSun, WeidongAuthor
Li, ShuguangAuthor
Chen, YadongAuthor
Li, YujingAuthor
Year2002 (July)Volume110
Issue4
PublisherUniversity of Chicago Press
DOIdoi:10.1086/340632Search in ResearchGate
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Mindat Ref. ID163927Long-form Identifiermindat:1:5:163927:2
GUID0
Full ReferenceSun, Weidong, Li, Shuguang, Chen, Yadong, Li, Yujing (2002) Timing of Synorogenic Granitoids in the South Qinling, Central China: Constraints on the Evolution of the Qinling‐Dabie Orogenic Belt. The Journal of Geology, 110 (4) 457-468 doi:10.1086/340632
Plain TextSun, Weidong, Li, Shuguang, Chen, Yadong, Li, Yujing (2002) Timing of Synorogenic Granitoids in the South Qinling, Central China: Constraints on the Evolution of the Qinling‐Dabie Orogenic Belt. The Journal of Geology, 110 (4) 457-468 doi:10.1086/340632
In(2002, July) The Journal of Geology Vol. 110 (4) University of Chicago Press

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Li, Shuguang, Sun, Weidong (1996) A Middle Silurian-Early Devonian Magmatic Arc in the Qinling Mountains of Central China: A Discussion. The Journal of Geology, 104 (4) 501-503 doi:10.1086/629843
Xu, Bei, Grove, M, Wang, Changqiu, Zhang, Lifei, Liu, Shuwen (2000) 40Ar/39Ar thermochronology from the northwestern Dabie Shan: constraints on the evolution of Qinling–Dabie orogenic belt, east-central China. Tectonophysics, 322 (3) 279-301 doi:10.1016/s0040-1951(00)00092-5
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Weidong Sun, Williams, I.S., and Shuguang Li (2002): Carboniferous and Triassic eclogites in the western Dabie Mountains, east-central China: evidence for protracted convergence of the North and South China Blocks. Journal of Metamorphic Geology 20(9), 873-886.
Liu, Jun-Feng, Li, Chao, Sun, Yong, Sun, Wei-Dong (2015) Melt percolation in the Songshugou ultramafic massif of the Qinling orogenic belt, Central China. International Geology Review, 57 (9) 1326-1339 doi:10.1080/00206814.2014.990525
Xiao, Bing; Li, Qiugen; He, Siyao; Chen, Xu; Liu, Shuwen; Wang, Zongqi; Xu, Xueyi; Chen, Junlu (2017) Contrasting geochemical signatures between Upper Triassic Mo-hosting and barren granitoids in the central segment of the South Qinling orogenic belt, central China: Implications for Mo exploration. Ore Geology Reviews, 81. doi:10.1016/j.oregeorev.2016.06.006
Wu, Yuan-Bao, Zheng, Yong-Fei (2013) Tectonic evolution of a composite collision orogen: An overview on the Qinling–Tongbai–Hong'an–Dabie–Sulu orogenic belt in central China. Gondwana Research, 23 (4) 1402-1428 doi:10.1016/j.gr.2012.09.007
Bao, Zhiwei, Wang, Christina Yan, Zeng, Lingjun, Sun, Weidong, Yao, Junming (2015) Slab break-off model for the Triassic syn-collisional granites in the Qinling orogenic belt, Central China: Zircon U-Pb age and Hf isotope constraints. International Geology Review, 57 (4) 492-507 doi:10.1080/00206814.2015.1017777
SU, Li (2005) Petrogenesis of Songshugou dunite body in the Qinling orogenic belt, Central China: Constraints from geochemis-try and melt inclusions. Science in China Series D, 48 (8). 1146pp. doi:10.1360/03yd0037
Zhang, Yong, Jia, Dong, Shen, Li, Yin, Hongwei, Chen, Zhuxin, Li, Haibin, Li, Zhigang, Sun, Chuang (2015) Provenance of detrital zircons in the Late Triassic Sichuan foreland basin: constraints on the evolution of the Qinling Orogen and Longmen Shan thrust-fold belt in central China. International Geology Review, 57 (14) 1806-1824 doi:10.1080/00206814.2015.1027967
Sun, Weidong, Williams, I. S., Li, Shuguang (2002) Carboniferous and Triassic eclogites in the western Dabie Mountains, east-central China: evidence for protracted convergence of the North and South China Blocks. Journal of Metamorphic Geology, 20 (9) 873-886 doi:10.1046/j.1525-1314.2002.00418.x
 
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