Dissolution of Quartz, Albite, and Orthoclase in H2O-Saturated Haplogranitic Melt at 800°C and 200 MPa: Diffusive Transport Properties of Granitic Melts at Crustal Anatectic Conditions
- 31 August 2005
- journal article
- Published by Oxford University Press (OUP) in Journal of Petrology
- Vol. 47 (2), 231-254
- https://doi.org/10.1093/petrology/egi073
Abstract
No abstract availableThis publication has 60 references indexed in Scilit:
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