Cenozoic thermo-tectonic evolution of the Gangdese batholith constrained by low-temperature thermochronology
Gangdese batholith in the southern Lhasa block is a key location for exploring the Tibetan Plateau uplift and exhumation history. We present the new low-temperature thermochronological data from two north-south traverses in the central Gangdese batholith to reveal their cooling histories and corresp...
| Main Authors: | , , , , , |
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| Format: | Journal Article |
| Published: |
Elsevier BV
2015
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| Online Access: | http://hdl.handle.net/20.500.11937/14690 |