Chapter 11 - Diversification of Magmas - Faculty web pages
Chapter 11 - Diversification of Magmas - Faculty web pages
Chapter 11 - Diversification of Magmas - Faculty web pages
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Langmuir Model<br />
<br />
<br />
Thermal gradient at wall and cap produces variation in %<br />
crystallization<br />
Compositional convection produces evolved magmas from<br />
boundary layer to cap<br />
Figure <strong>11</strong>-12<br />
12 Formation <strong>of</strong> boundary layers along<br />
the walls and top <strong>of</strong> a magma chamber. From<br />
Winter (2001) An Introduction to Igneous and<br />
Metamorphic Petrology. Prentice Hall
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