Melting of the Meso-Neoproterozoic juvenile crust for the origin of the Late Triassic Mo mineralization in South Qinling, central China: Evidence from geochronology and geochemistry of the Yangmugou deposit

2019 ◽  
Vol 174 ◽  
pp. 109-125 ◽  
Author(s):  
Lei Chen ◽  
Zhen Yan ◽  
Xianqing Guo ◽  
Changlei Fu
AAPG Bulletin ◽  
2017 ◽  
Vol 101 (01) ◽  
pp. 95-117 ◽  
Author(s):  
Renchao Yang ◽  
Zhijun Jin ◽  
A.J. (Tom) van Loon ◽  
Zuozhen Han ◽  
Aiping Fan

2021 ◽  
Author(s):  
Zhenhua Xue ◽  
Wei Lin ◽  
et al.

Text: Basic principles of anisotropy of magnetic susceptibility (AMS); Figure S1: Photographs of supplementary shearing indicators of the structural kinematics; Figure S2: Complete magnetic hysteresis data set for specimen selected from 34 sites; Figure S3: Measurements of isothermal remanent magnetization of specimen selected from 34 representative sites of the Bikou Terrane; Figure S4: Thermo-magnetic experiments of specimen selected from 12 representative sites; Figure S5: Mrs/Ms versus Hcr/Hc diagram from the selected specimen of the representative sites to define the size of magnetite; Figure S6: Stereographic projection of the AMS directional fabrics and structural fabrics.


2016 ◽  
Vol 155 (4) ◽  
pp. 893-906 ◽  
Author(s):  
CHUANBO SHEN ◽  
DI HU ◽  
CHUN SHAO ◽  
LIANFU MEI

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.


2000 ◽  
Vol 105 (B6) ◽  
pp. 13339-13364 ◽  
Author(s):  
Bradley R. Hacker ◽  
Lothar Ratschbacher ◽  
Laura Webb ◽  
Michael O. McWilliams ◽  
Trevor Ireland ◽  
...  

2018 ◽  
Vol 114 ◽  
pp. 64-75 ◽  
Author(s):  
Jinxi Li ◽  
Zhiwu Li ◽  
Shugen Liu ◽  
Bo Ran ◽  
Yuehao Ye ◽  
...  

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