scholarly journals Post-collisional orogen-parallel extension in the Trans-North China Orogen: Evidence from syn-kinematic pegmatite dikes

2022 ◽  
Vol 368 ◽  
pp. 106503
Author(s):  
Yunjian Li ◽  
Guang Zhu ◽  
Chengchufan Gu ◽  
Cheng Liu ◽  
Shuai Zhang ◽  
...  
Keyword(s):  
North China ◽  
Collisional Orogen ◽  
Parallel Extension

Parallel Extension Tectonics: Mechanism of Early Cretaceous thinning and destruction of the lithosphere of the North China Craton

2020 ◽  
Vol 36 (8) ◽  
pp. 2331-2343
Author(s):  
LIU JunLai ◽  
◽  
NI JinLong ◽  
CHEN XiaoYu ◽  
CRADDOCK JP ◽  
...  
Keyword(s):  
Early Cretaceous ◽  
North China Craton ◽  
North China ◽  
The North ◽  
Parallel Extension

Coesite from quartz-jadeitite in the Dabie Mountains, Eastern China

1996 ◽  
Vol 60 (401) ◽  
pp. 659-662 ◽  
Author(s):  
Wen Su ◽  
Shutong Xu ◽  
Laili Jiang ◽  
Yican Liu
Keyword(s):  
North China ◽  
Eastern China ◽  
Dabie Mountains ◽  
Collisional Orogen ◽  
The North ◽  
Ophiolitic Mélange ◽  
Continental Plate ◽  
Thrust Belts ◽  
Fold And Thrust Belt ◽  
Back Arc

The Dabie Mountains is a collisional orogen between the North China and Yantze Continental plates. It is composed, from south to north, of the foreland fold and thrust belt alternated with molasse basin, the subducted cover and basement of the Yangtze continental plate, the meta-ophiolitic melange belt, the forearc meta-flysch nappe (bounded by southward and northward thrust belts) in which there may be a buried volcanic arc and a relict back-arc basin (Fig. 1A) (Xu et al., 1992a, 1994).

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