Correlation of Himalayan exhumation rates and Asian monsoon intensity
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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
| Collections | ANU 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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| File | Description | Size | Format | Image |
|---|---|---|---|---|
| 01_Clift_Correlation_of_Himalayan_2008.pdf | 1.05 MB | Adobe PDF |  |
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