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Correlation of Himalayan exhumation rates and Asian monsoon intensity

Clift, Peter D.; Hodges, Kip V; Heslop, David; Hannigan, Robyn; Van Long, Hoang; Calves, Gerome

Description

Although most data suggest that the India-Eurasia continental collision began 45-55 Myr ago, the architecture of the Himalayan-Tibetan orogen is dominated by deformational structures developed in the Neogene period (<23 Myr ago). The stratigraphic record

CollectionsANU Research Publications
Date published: 2008
Type: Journal article
URI: http://hdl.handle.net/1885/29309
Source: Nature Geoscience
DOI: 10.1038/ngeo351

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