2005
DOI: 10.1111/j.1755-6724.2005.tb00864.x
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Numerical Modeling of Basin‐Range Tectonics Related to Continent‐Continent Collision

Abstract: Continentsontinent collision is the most important driving mechanism for the occurrence of various geological processes in the continental lithosphere. How to recognize and determine continent-continent collision. especially its fourdimensional temporal-spatial evolution, is a subject that geological communities have long been concerned about and studied, Continent-continent collision is mainly manifested by strong underthrusting (subduction) of the underlying block along an intracontinental subduction zone an… Show more

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Cited by 2 publications
(1 citation statement)
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“…Previous studies suggest that SE China underwent a complicated tectonic evolution from the Paleo-Tethys regime to the Pacific regime and then to an intracontinental tectonic setting (Ren et al, 1998(Ren et al, , 1999Ren and Xiao, 2004;Wang and Chen, 2004;Cui et al, 2005;Zhou and Li, 2000;Shu and Charvet, 1996;Shu et al, 2003). Paleo-Tethys is a sub-E-W-extending tectonic domain; during the pre-Triassic, the SE China block (including the Wuyishan and the Nanling Ranges) belonged to the northern Tethys regime situated in southern Laurasian Land.…”
Section: Early Mesozoic Basin-granite Frameworkmentioning
confidence: 99%
“…Previous studies suggest that SE China underwent a complicated tectonic evolution from the Paleo-Tethys regime to the Pacific regime and then to an intracontinental tectonic setting (Ren et al, 1998(Ren et al, , 1999Ren and Xiao, 2004;Wang and Chen, 2004;Cui et al, 2005;Zhou and Li, 2000;Shu and Charvet, 1996;Shu et al, 2003). Paleo-Tethys is a sub-E-W-extending tectonic domain; during the pre-Triassic, the SE China block (including the Wuyishan and the Nanling Ranges) belonged to the northern Tethys regime situated in southern Laurasian Land.…”
Section: Early Mesozoic Basin-granite Frameworkmentioning
confidence: 99%