The thermal evolution of the Nyainqentanglha Shan: Evidence for a long-lived, lower crustal magmatic system in Southern Tibet

Journal of Asian Earth Sciences

Volumn 19, Issue 3A, 2001, Pages 12-13

  D'Andrea, J ^a   Harrison, T M ^a   Grove, M ^a   Lin, D ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0035029851     PISSN: 13679120     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Conference Paper

References (4)

1. The Zedong window: A record of superposed tertiary convergence in southeastern Tibet
2. Southern limit of mantle-derived geothermal helium emissions in Tibet: Implications for lithospheric structure
3. Implications of crustal property variations for models of Tibetan plateau evolution
4. Seismic and rheological constraints on the thermal state of Tibetan plateau upper mantle: Implications for melt production, mantle delamination, and large-scale tectonics