A bound on the viscosity of the Tibetan crust from the horizontality of palaeolake shorelines
Palaeoshorelines around four large lakes in central Tibet record a latest-Pleistocene-to-Holocene high stand during which the lakes were filled 150–200 m more deeply than they are at present. GPS measurements of shoreline elevations around Zhari Namtso show that they are horizontal to within ±2 m at...
| Main Authors: | , , , |
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| Other Authors: | |
| Format: | Article |
| Language: | en_US |
| Published: |
Elsevier B.V.
2014
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| Online Access: | http://hdl.handle.net/1721.1/90571 https://orcid.org/0000-0002-1657-2084 |