Late Neoproterozoic magmatism in South Qinling, Central China: Geochemistry, zircon U-Pb-Lu-Hf isotopes and tectonic implications

2016 ◽  
Vol 683 ◽  
pp. 43-61 ◽  
Author(s):  
Ruirui Wang ◽  
Zhiqin Xu ◽  
M. Santosh ◽  
Yuan Yao ◽  
Li'e Gao ◽  
...  
Keyword(s):  
Central China ◽  
Hf Isotopes ◽  
South Qinling ◽  
Tectonic Implications ◽  
Late Neoproterozoic ◽  
Neoproterozoic Magmatism

Chronology and tectonic implications of Neoproterozoic blocks in the South Qinling Orogenic Belt, Central China

2016 ◽  
Vol 30 ◽  
pp. 24-47 ◽  
Author(s):  
Fangyang Hu ◽  
Shuwen Liu ◽  
M. Santosh ◽  
Zhengbin Deng ◽  
Wei Wang ◽  
...  
Keyword(s):  
Orogenic Belt ◽  
Central China ◽  
The South ◽  
Qinling Orogenic Belt ◽  
South Qinling ◽  
Tectonic Implications

Thermochronology quantifying exhumation history of the Wudang Complex in the South Qinling Orogenic Belt, central China

2016 ◽  
Vol 155 (4) ◽  
pp. 893-906 ◽  
Author(s):  
CHUANBO SHEN ◽  
DI HU ◽  
CHUN SHAO ◽  
LIANFU MEI
Keyword(s):  
Distance Effect ◽  
Central China ◽  
The Tibetan Plateau ◽  
Yangtze Craton ◽  
Long Distance ◽  
South Qinling ◽  
The North ◽  
The Pacific ◽  
History Of ◽  
Exhumation History

AbstractThe Wudang Complex located in the central part of South Qinling, has been inferred to be a segment of the Yangtze Craton involved in the orogen. In this study, the cooling/exhumation history of the Wudang Complex is revealed through combined published geochronology data and new apatite fission-track results. Three rapid exhumation episodes related to relevant geodynamic events have been identified. Previous40Ar–39Ar and (U–Th)/He data indicate that the most significant exhumation, induced by the collision between the North and South China Blocks, occurred fromc.237 to 220 Ma after long-term subsidence and sedimentation of the passive continental margin. The second exhumation event, related to the long-distance effect of the Pacific subduction, occurred during the period fromc.126 to 90 Ma. Following the late Cretaceous – Eocene peneplanation stage, the final late Cenozoic exhumation sincec.15 Ma may be attributed to the combined effect of the eastward growth of the Tibetan Plateau uplift and the Asian monsoon.

Seismic Imaging of Lithosphere Structure and Upper Mantle Deformation Beneath East‐Central China and Their Tectonic Implications

2018 ◽  
Vol 123 (4) ◽  
pp. 2856-2870 ◽  
Author(s):  
Hongyi Li ◽  
Xiaodong Song ◽  
Qingtian Lü ◽  
Xiaoyu Yang ◽  
Yangfan Deng ◽  
...  
Keyword(s):  
Upper Mantle ◽  
Seismic Imaging ◽  
Central China ◽  
East Central ◽  
Lithosphere Structure ◽  
Tectonic Implications
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