Tohver, Eric 
; Teixeira, Wilson ; Geraldes, Mauro Cesar ; Bettencourt, Jorge Silva
Source: Abstracts with Programs, Geological Society of America. Conference titles: Geological Society of America. Annual Meeting. Unidade: IGC
Subjects: OROGÊNESE, TOPOGRAFIA, TERMOCRONOLOGIA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
TOHVER, Eric et al. Beneath the topography: comparative U/PB and 40AR/39AR thermochronology of the exhumed grenvillian crust of north and South America and implications for orogenic structure. Abstracts with Programs, Geological Society of America. Oregon: Instituto de Geociências, Universidade de São Paulo. Disponível em: https://gsa.confex.com/gsa/2005AM/webprogram/Paper92100.html. Acesso em: 07 nov. 2024. , 2005APA
Tohver, E., Teixeira, W., Geraldes, M. C., & Bettencourt, J. S. (2005). Beneath the topography: comparative U/PB and 40AR/39AR thermochronology of the exhumed grenvillian crust of north and South America and implications for orogenic structure. Abstracts with Programs, Geological Society of America. Oregon: Instituto de Geociências, Universidade de São Paulo. Recuperado de https://gsa.confex.com/gsa/2005AM/webprogram/Paper92100.htmlNLM
Tohver E, Teixeira W, Geraldes MC, Bettencourt JS. Beneath the topography: comparative U/PB and 40AR/39AR thermochronology of the exhumed grenvillian crust of north and South America and implications for orogenic structure [Internet]. Abstracts with Programs, Geological Society of America. 2005 ; 37( 7):[citado 2024 nov. 07 ] Available from: https://gsa.confex.com/gsa/2005AM/webprogram/Paper92100.htmlVancouver
Tohver E, Teixeira W, Geraldes MC, Bettencourt JS. Beneath the topography: comparative U/PB and 40AR/39AR thermochronology of the exhumed grenvillian crust of north and South America and implications for orogenic structure [Internet]. Abstracts with Programs, Geological Society of America. 2005 ; 37( 7):[citado 2024 nov. 07 ] Available from: https://gsa.confex.com/gsa/2005AM/webprogram/Paper92100.html
