Chapter 11 - Diversification of Magmas - Faculty web pages

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

$Math 362 Problem Set #9 â€“ Solution 27 April 2012 - Faculty web ...$

Flow differentiation - Concentration of coarse phenocrysts toward center of dikes and sills
Volatile Transport - separate vapor phase coexists with magma 1. Vapor released by heating of hydrated or carbonated wall rocks 2. As a volatile-bearing magma rises and pressure is reduced, magma becomes saturated in the vapor, and a free vapor phase will be released Produces hydrothermal effects such as alkali metasomatism called fenitization
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: Mechanisms that facilitate the sepa
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 and 34: In Situ Differentiation Processes
Page 35 and 36: Thermogravitational diffusion Stabl
Page 37 and 38: Detecting and assessing assimilatio
Page 39: Tectonic-Igneous Associations Mid-

Chapter 11 - Diversification of Magmas - Faculty web pages

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