Chapter 11 - Diversification of Magmas - Faculty web pages

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$Math 361 Problem Set #5 Due 5 October 2012 - Faculty web pages$

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The Soret Effect Thermal diffusion = Soret effect Heavy elements/molecules migrate toward the colder end and lighter ones to the hotter end of the gradient
Thermogravitational diffusion Stable and persistent stagnant boundary layers occur near the top and sides of magma chambers Figure 11-11. Schematic section through a rhyolitic magma chamber undergoing convection-aided in-situ differentiation. After Hildreth (1979). Geol. Soc. Amer. Special Paper, 180, 43-75.
Page 1 and 2: Chapter 11: Diversification of Magm
Page 3 and 4: Magmatic Differentiation Two essen
Page 5 and 6: Eutectic Melting Eutectic point = t
Page 7 and 8: Critical Melt Fraction Separation
Page 9 and 10: Factors affecting separation of mel
Page 11 and 12: Fractional Crystallization Proces
Page 13 and 14: Gravity settling - Ternary Phase Di
Page 15 and 16: Olivine in basalt Olivine (ρ( s =
Page 17 and 18: Stokes’ Law is overly simplified
Page 19 and 20: Mechanisms that facilitate the sepa
Page 21 and 22: Volatile Transport - separate vapor
Page 23 and 24: Volatile release increases P - frac
Page 25 and 26: Hornblende retrograde boiling Silve
Page 27 and 28: Liquid Immiscibility - Italian Sala
Page 29 and 30: Magma Mixing End member mixing in
Page 31 and 32: Assimilation Incorporation of wal
Page 33: In Situ Differentiation Processes
Page 37 and 38: Detecting and assessing assimilatio
Page 39: Tectonic-Igneous Associations Mid-

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