U–Pb dating on single detrital zircon grains from the Triassic Songpan–Ganze flysch (Central China): provenance and tectonic correlations

1997 ◽  
Vol 152 (1-4) ◽  
pp. 217-231 ◽  
Author(s):  
O. Bruguier ◽  
J.R. Lancelot ◽  
J. Malavieille
Keyword(s):  
Detrital Zircon ◽  
Central China

Detrital zircon (U–Th)/He thermochronometry of the Mesozoic Daba Shan Foreland Basin, central China: Evidence for timing of post-orogenic denudation

2012 ◽  
Vol 570-571 ◽  
pp. 65-77 ◽  
Author(s):  
Yuntao Tian ◽  
Nansheng Qiu ◽  
Barry P. Kohn ◽  
Chuanqing Zhu ◽  
Shengbiao Hu ◽  
...  
Keyword(s):  
Detrital Zircon ◽  
Foreland Basin ◽  
Central China

scholarly journals Detrital zircon trace elements from the Mesozoic Jiyuan Basin, central China and its implication on tectonic transition of the Qinling Orogenic Belt

2019 ◽  
Vol 11 (1) ◽  
pp. 125-139 ◽  
Author(s):  
Min Wang ◽  
Wenfei Guo ◽  
Wentao Yang
Keyword(s):  
Trace Elements ◽  
Detrital Zircon ◽  
Middle Triassic ◽  
Tectonic Setting ◽  
Central China ◽  
Qinling Orogen ◽  
Tectonic Transition ◽  
Lithospheric Extension ◽  
Mountain System ◽  
Zircon Trace Elements

AbstractThe Qinling Orogen and the Jiyuan Basin constitute a basin-mountain system during the Early Mesozoic. Therefore, sediments from the Jiyuan Basin can be used to deduce the orogenic process of the Qinling Orogen. This paper attempts to use detrital zircon trace elements with ages ranging from the Late Carboniferous to the Middle Triassic that were obtained from the Jiyuan Basin to discuss the tectonic evolution of Qinling Orogen. On the tectonic setting discriminating diagrams, most grains are concentrated in convergent continental margins/orogenic settings,whereas the remaining samples (268 Ma, 265Ma, 264 Ma and 254Ma) are plotted in anorogenic field. Compared to the Early Paleozoic (400-500Ma) zircons, 306Ma and 281Ma grains represent higher Th/ Nb ratios, which might be related to the Mianlve oceanic crust subduction. The lower Th/Nb ratios containing 268 Ma, 265Ma, 264 Ma and 254Ma grains might indicate lithospheric extension subsequently. The final continent-continent collision between South China and North China blocks took place after the Middle Triassic (242Ma).

Stratigraphic and U‐Pb SHRIMP Detrital Zircon Evidence for a Neoproterozoic Continental Arc, Central China: Rodinia Implications

2006 ◽  
Vol 114 (5) ◽  
pp. 627-636 ◽  
Author(s):  
Peter Druschke ◽  
Andrew D. Hanson ◽  
Quanren Yan ◽  
Zhongqi Wang ◽  
Tao Wang
Keyword(s):  
Detrital Zircon ◽  
Central China ◽  
Continental Arc

Surface brightening in eastern and central China since the implementation of the Clean Air Action in 2013: causes and implications

2020 ◽  
Author(s):  
Hongrong Shi ◽  
Jinqiang Zhang ◽  
Bin Zhao ◽  
Xiangao Xia ◽  
Bo Hu ◽  
...  
Keyword(s):  
Central China ◽  
Clean Air
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