Chapter 11 - Diversification of Magmas - Faculty web pages

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Comingled Basalt-Rhyolite Mt. McLoughlin, , Oregon Figure 11-8 From Winter (2001) An Introduction to Igneous and Metamorphic Petrology. Prentice Hall Basalt pillows accumulating at the bottom of granitic magma chamber Vinalhaven Island, Maine
Assimilation Incorporation of wall rocks, xenoliths Assimilation by melting is limited by the heat available in the magma
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: Magma Mixing End member mixing in
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-

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