S. Lister (2012), The collision of India with Asia, J. Geodyn., 56-57, 7-17, doi:10.1016/j.jog.2011.06.006.White, L. T., and G. S. Lister (2012), The collision of India with Asia, J. Geodyn., 56-57, 7-17.White, L., Lister, G., 2012. The collision of India with ...
Convergence between the Indian and Asian plates has reshaped large parts of Asia, changing regional climate and biodiversity, yet geodynamic models fundamentally diverge on how convergence was accommodated since the India–Asia collision. Here we report palaeomagnetic data from the Burma Terrane, which...
The timing of continental collision between India and Asia has been controversial for a long time because of the difficulty in screening isotopic ages for different types of tectonothermal event along the convergent continental boundary. After distinguishing the collisional orogeny from the precollisional...
The collision between India and Eurasia mobilizes multiple processes of continental tectonics. However, how deformation develops within the lithosphere across the Tibetan Plateau is still poorly known and a synoptic view is missing. Here, we exploit an extensive geodetic observatory to resolve the kinema...
collision-induced CO2emission flux associated with the evolving Neo-Tethyan to continental subduction over the Cenozoic. The correlation between our modelled CO2emission rates and the global atmospheric CO2curve is consistent with the hypothesis that the India-Asia collision was the primary driver of ...
The South China Sea (SCS) is one of the biggest marginal seas in the western Pacific region. Affected by the India-Eurasia collision to the northwest (Morley, 2002), the subduction of the Pacific Plate and then the compression from the Philippine Sea plate in the east (Zhou et al., 2002...
Even though we have not succeeded in obtaining conclusive data about the exact timing of phases of rapid uplift of the Tibetan Plateau, it is most likely that the major phase of uplift occurred during the Late Oligocene. Introduction Continental collision between India and Asia resulted in crustal...
The North China craton is one of the oldest continental nuclei on earth (Liu et al., 1992), originated from the collision between the Yanliao and Ordos blocks in the Paleoproterozoic (1.85 Ga, Fig. 2C, Zhao, et al., 2005). In the Mesozoic, this craton was reactivated, with lithospheri...
Kinematic model of active deformation in central Asia. Geophys. Res. Lett. 20, 895–898 (1993). Google Scholar Copley, A., Avouac, J.-P. & Royer, J.-Y. India-Asia collision and the Cenozoic slowdown of the Indian plate: Implications for the forces driving plate motions. J. Geophys...
Kroon, D., Steens, T. & Troelstra, S. R. Onset of monsoonal related upwelling in the western Arabian Sea as revealed by planktonic foraminifers.Proc. ODP Sci. Res.117, 257–263 (1991) Google Scholar Rowley, D. B. Age of initiation of collision between India and Asia: a review of ...