scholarly journals Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks: Comment and Reply: REPLY

Geology ◽  
2006 ◽  
Vol 34 (1) ◽  
pp. e107-e108
Author(s):  
A. L. Weislogel ◽  
S. A. Graham ◽  
E. Z. Chang ◽  
J. L. Wooden ◽  
G. E. Gehrels ◽  
...  
Keyword(s):  
South China ◽  
Detrital Zircon ◽  
Late Triassic ◽  
Sedimentary Record ◽  
The North ◽  
North And South

Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks

Geology ◽  
2006 ◽  
Vol 34 (2) ◽  
pp. 97 ◽  
Author(s):  
Amy L. Weislogel ◽  
Stephan A. Graham ◽  
Edmund Z. Chang ◽  
Joeseph L. Wooden ◽  
George E. Gehrels ◽  
...  
Keyword(s):  
South China ◽  
Detrital Zircon ◽  
Late Triassic ◽  
Sedimentary Record ◽  
The North ◽  
North And South

Sedimentary record of the collision of the North and South China cratons : New insights from the Western Hubei Trough

2018 ◽  
Vol 54 (6) ◽  
pp. 3335-3348 ◽  
Author(s):  
Binsong Zheng ◽  
Chuanlong Mou ◽  
Xiuping Wang ◽  
Zhaohui Xiao ◽  
Yao Chen
Keyword(s):  
South China ◽  
Sedimentary Record ◽  
The North ◽  
Western Hubei ◽  
North And South

Palaeomagnetism, North China and South China collision, and the Tan-Lu fault

1990 ◽  
Vol 331 (1620) ◽  
pp. 589-598 ◽  
Keyword(s):  
South China ◽  
North China ◽  
Eastern China ◽  
Early Jurassic ◽  
Late Triassic ◽  
Polar Wander ◽  
The North ◽  
Indosinian Orogeny ◽  
North And South ◽  
Transcurrent Faults

Refined Apparent Polar Wander (APW) paths for the North and South China Blocks (ncb and scb) are presented and the collision between the NCB and SCB discussed. We suggest that the amalgamation of the NCB and SCB was completed in the late Triassic-early Jurassic, during the Indosinian Orogeny. This proposed timing is based on an analysis of palaeomagnetic signatures relating to continental collisions, such as the convergence of palaeolatitude, deflections of declination, hairpin-like loops in and superposition of APW paths. Like the Cenozoic India—Eurasia collision, the Mesozoic NCB- SCB collision reactivated ancient faults in eastern China, converting some of them into transcurrent faults, of which the Tan-Lu fault is the most famous.

Preliminary Phanerozoic polar wander paths for the North and South China blocks

Nature ◽  
1985 ◽  
Vol 313 (6002) ◽  
pp. 444-449 ◽  
Author(s):  
Jin-lu Lin ◽  
M. Fuller ◽  
Wen-you Zhang
Keyword(s):  
South China ◽  
Polar Wander ◽  
The North ◽  
North And South

Jurassic paleomagnetic constraints on the collision of the North and South China Blocks

1992 ◽  
Vol 19 (6) ◽  
pp. 577-580 ◽  
Author(s):  
Zhenyu Yang ◽  
Vincent Courtillot ◽  
Jean Besse ◽  
Xinghua Ma ◽  
Lisheng Xing ◽  
...  
Keyword(s):  
South China ◽  
The North ◽  
North And South

Neoproterozoic arc volcanic rocks of the Nanping-Ninghua tectonic belt, South China: Implications for the collision between the North and South Wuyi blocks

2018 ◽  
Vol 54 (4) ◽  
pp. 2679-2692 ◽  
Author(s):  
Yang Jiang ◽  
Xilin Zhao ◽  
Yanjie Zhang ◽  
Guangfu Xing ◽  
Mincheng Xu ◽  
...  
Keyword(s):  
South China ◽  
Volcanic Rocks ◽  
The North ◽  
Tectonic Belt ◽  
North And South
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