Chapter 18: Granitoid Rocks - Faculty web pages

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Transitional - Post-orogenic (after true orogenic event); 10-100 Maafter compressive deformation stopped. Emplaced during uplift andextensional collapse following orogeny
Himalayas – Continent – continent collisionFigure <strong>18</strong>-7. Schematic cross section of the Himalayas showing the dehydration and partialmelting zones that produced the leucogranites.After France-Lanord and Le Fort (1988) Trans. Roy. Soc. Edinburgh, 79, <strong>18</strong>3-195. Winter (2001) An Introduction to Igneous andMetamorphic Petrology. Prentice Hall.
Page 1 and 2: Chapter 18: Granitoid Rocks“Grani
Page 3 and 4: 2) Because the crust is solid in it
Page 5 and 6: Zircon Xenocrysts - Hard, refractor
Page 7 and 8: Alumina saturation: Peraluminous -
Page 9 and 10: Granitoid classification: S-I-A-M S
Page 11 and 12: Table 18-3. The S-I-A-M Classificat
Page 13: Anorogenic - magmatism within a pla

Chapter 18: Granitoid Rocks - Faculty web pages

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