The study of the orogenic effects of the Tibetan Plateau uplift on global climate during the Cenozoic has focused almost exclusively on the India-Asia collision zone, the Himalayas. The strong erosion in the Himalayas was assumed to be a primary driver of Cenozoic atmospheric CO[2] decline and global cooling predominantly...
Full ArticleCan East Asian Monsoon Enhancement Induce Global Cooling?
Eurasia Review
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