Two competing effects of volatiles on heat transfer in crystal-rich magmas: Thermal insulation vs defrosting

Journal of Petrology

Volumn 51, Issue 4, 2010, Pages 847-867

  Huber, Christian ^a   Bachmann, Olivier ^b   Manga, Michael ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

^b UNIVERSITY OF WASHINGTON   (United States)

Author keywords

Defrosting; Intrusion; Magma chamber; Mush; Thermal insulation; Volatiles

Indexed keywords

CHEMICAL COMPOSITION; ENTHALPY; EXSOLUTION; HEAT TRANSFER; IGNEOUS INTRUSION; IGNIMBRITE; MAGMA CHAMBER; PARTIAL MELTING; REMOBILIZATION; RHEOLOGY; THERMAL EVOLUTION; UNDERPLATING; VOLATILE SUBSTANCE;

EID: 77952722366     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egq003     Document Type: Article

References (34)

1. Assael, M. J., Bekou, E., Giakoumakis, D., Friend, D. G., Killeen, M. A., Millat, J. & Nagashima, A. (2000). Experimental data for the viscosity and thermal conductivity of water and steam. Journal of Physical and Chemical Reference Data 29,141-166.
2. Bachmann, O. & Bergantz, G. W. (2006). Gas percolation in uppercrustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies. Journal of Volcanology and Geothermal Research 149,85-102.
3. Bagdassarov, N. & Dingwell, D. (1994). Thermal properties of vesicular rhyolite. Journal of Volcanology and Geothermal Research 60, 179-191.
4. Bear, J. (1972). Dynamics of Fluids in Porous Media. NewYork: Dover.
5. Brooks, R. H. & Corey, A. T. (1964). Hydraulic Properties of Porous Media. Hydrology Paper 3. Fort Collins: Colorado State University.
6. Cardoso, S. S. S. & Woods, A. W. (1999). On convection in a volatilesaturated magma. Earth and Planetary Science Letters 168, 301-310.
7. Carrigan, C. R. (1988). Biot number and thermos bottle effect: Implications for magma-chamber convection. Geology 16, 771-774.
8. Christiansen, E. H. (2005). Contrasting processes in silicic magma chambers: evidence from very large volume ignimbrites. Geological Magazine 142, 669-681.
9. Christiansen, E. N. & McCurry, M. (2008). Contrasting origins of Cenozoic silicic volcanic rocks from the western Cordillera of the United States. Bulletin of Volcanology 70,251-267.
10. Couch, S., Sparks, R. S. J. & Carroll, M. R. (2001). Mineral disequilibrium in lavas explained by convective self-mixing in open magma chambers. Nature 411, 1037-1039.
11. Davaille, A. & Jaupart, C. (1993). Transient high-Rayleigh number thermal convection with large viscosity variations. Journal of Fluid Mechanics 253,141-166.
12. Dingwell, D. B., Bagdassarov, N. S., Bussod, J. & Webb, S. L. (1993). Magma rheology. In: Luth, R. W. (ed.) Experiments at High Pressure and Applications to the Earth's Mantle. Mineralogical Association of Canada, Short Course Handbooks 21,131-196.
13. Eichelberger, J. C. (1980).Vesiculation of mafic magma during replenishment of silicic magma reservoirs. Nature 288, 446-450.
14. Ghiorso, M. S. & Sack, R. O. (1995). Chemical mass transfer in magmatic processes IV: A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquidsolid equilibria in magmatic systems at elevated temperatures and pressures. Contributions to Mineralogy and Petrology 119, 197-212.
15. Halbach, H. & Chatterjee, N. D. (1982). An empirical RedlichKwong equation of state for water to 1000°C and 200 kbar. Contributions to Mineralogy and Petrology 79,337-345.
16. Hashin, Z. & Shtrikman, S. (1963). A variational approach to the theory of elastic behavior of multiphase materials. Journal of the Mechanics and Physics of Solids 11,127-140.
17. Huber, C., Bachmann, O. & Manga, M. (2009). Homogenization processes in silicic magma chambers by stirring and latent heat buffering. Earth and Planetary Science Letters 283, 38-47.
18. Huppert, H. E. & Sparks, R. S. J. (1980). The fluid dynamics of a basaltic magma chamber replenishment by influx of hot, dense ultrabasic magma. Contributions to Mineralogy and Petrology 75, 279-289.
19. Huppert,H.E.,Sparks,R.S.J.&Turner,J.S. (1982).Effectsofvolatiles on mixing in calc-alkaline magma systems. Nature 332, 554-557.
20. Jellinek, A. M., Kerr, R. C. & Griffiths, R. W. (1999). Mixing and compositional stratification produced by natural convection: 1. Experiments and their applications to Earth's core and mantle. Journal of Geophysical Research 104, 7183-7201.
21. Karlstrom, L., Dufek, J. & Manga, M. (2009). Organization of volcanic plumbing through magmatic lensing by magma chambers and volcanic loads. Journal of Geophysical Research 114, B10204, doi:10.1029/2009JB006339.
22. Koyaguchi, T. & Kaneko, K. (1999). A two-stage thermal evolution model of magmas in continental crust. Journal of Petrology 40, 241-254.
23. Koyaguchi, T. & Kaneko, K. (2000). Thermal evolution of silicic magma chambers after basalt replenishment. Transactions of the Royal Society of Edimburgh 91, 47-60.
24. Lemmon, E. W., McLinden, M. O. & Friend, D. G. (2003). Thermophysical Properties of Fluid Systems. Gaithersburg, MD: National Institute of Standards and Technology.
25. Lindsay, J. M., Schmitt, A. K., Trumbull, R. B., De Silva, S. L., Siebel, W. & Emmermann, R. (2001). Magmatic evolution of the La Pacana caldera system, Central Andes, Chile: Compositional variation of two cogenetic, large-volume felsic ignimbrites. Journal of Petrology 42, 459-486.
26. Lipman, P. W. (2007). Incremental assembly and prolonged consolidation of Cordilleran magma chambers: Evidence from the Southern Rocky Mountain volcanic field. Geosphere 3,1-29.
27. Mahood, G. A. (1990). Second reply to comment of R.S.J. Sparks, H.E. Huppert, and C.J.N. Wilson on 'Evidence for long residence times of rhyolitic magma in the Long Valley magmatic system: the isotopic record in precaldera lavas of Glass Mountain'. Earth and Planetary Science Letters 99, 395-399.
28. Marsh, B. D. (1981). On the crystallinity, probability of occurrence, and rheology of lava and magma. Contributions to Mineralogy and Petrology 78, 85-98.
29. Murase, T. & McBirney, A. R. (1973). Properties of some common igneous rocks and their melts at high temperature. Geological Society of America Bulletin 84, 3563-3592.
30. Namiki, A., Hatakeyama, T., Toramaru, A., Kurita, K. & Sumita, I. (2003). Bubble size distributions in a convecting layer. Geophysical Research Letters 30, 2-4.
31. Parat, F., Holtz, F. & Feig, S. (2008). Pre-eruptive conditions of the Huerto Andesite (Fish Canyon system, San Juan volcanic field, Colorado): influence of volatiles (C-O-H-S) on phase equilibria and mineral composition. Journal of Petrology 49,911-935.
32. Reid,M.R.,Coath,C.D.,Harrison,T.M.&McKeegan,K.D. (1997). Prolonged residence times for the youngest rhyolites associated with Long Valley Caldera: 230Th-238U microprobe dating of young zircons. Earth and Planetary Science Letters 150, 27-39.
33. Snyder, D. (2000). Thermal effects of the intrusion of basaltic magma into a more silicic magma chamber and implications for eruption triggering. Earth and Planetary Science Letters 175,257-273.
34. Streck, M. & Grunder, A. (2008). Phenocryst-poor rhyolites of bimodal, tholeiitic provinces: the Rattlesnake Tuff and implications for mush extraction models. Bulletin of Volcanology 70, 385-401.