Zircon stability grids in crustal partial melts: implications for zircon inheritance
Author:
Funder
Ministerio de Ciencia e Innovación
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-021-01772-x.pdf
Reference45 articles.
1. Arzi AA (1978) Critical phenomena in the rheology of partially melted rocks. Tectonophysics 44:173–184
2. Bagdassarov NS, Dorfman AM, Dingwell DB (1996) Modelling of melt segregation processes by high-temperature centrifuging of partially molten granites.1. Melt extraction by compaction and deformation. Geophys J Int 127:616–626
3. Barboza SA, Bergantz GW (1998) Rheological transitions and the progress of melting of crustal rocks. Earth Planet Sci Lett 158:19–29
4. Bea F (1996) Controls on the trace element composition of crustal melts. Trans R Soc Edinb Earth Sci 87(133–41):33–42
5. Bea F (2010) Crystallization dynamics of granite magma chambers in the absence of regional stress: multiphysics modeling with natural examples. J Petrol 51:1541–1569
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