Effect of pressure on closure temperature of a trace element in cooling petrological systems
Author:
Funder
National Science Foundation
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-016-1327-8.pdf
Reference43 articles.
1. Albarède F (1995) Introduction to geochemical modeling. Cambridge University Press, Cambridge
2. Béjina F, Jaoul O, Liebermann RC (2003) Diffusion in minerals at high pressure: a review. Phys Earth Planet Interiors 139:3–20
3. Bjerg EA, Ntaflos T, Thöni M, Aliani P, Labudia CH (2009) Heterogeneous lithospheric mantle beneath northern Patagonia: evidence from Prahuaniyeu garnet- and spinelperidotites. J Petrol 50:1267–1298
4. Bloch E, Ganguly J, Hervig R, Cheng W (2015) 176Lu–176Hf geochronology of garnet I: experimental determination of diffusion kinetics of Lu3+ and Hf4+ in garnet, closure temperatures and geochronological implications. Contrib Miner Petrol 169:12
5. Brey G, Köhler T (1990) Geothermobarometry in four-phase lherzolites II. New thermobarometers, and practical assessment of existing thermobarometers. J Petrol 31:1353–1378
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