fig temperature pressure diagram showing the three major types of metamorphic facies series proposed by person 1973, 1994 winter 2001 an introduction to igneous and metamorphic petrology prentice hall
{"Image DocumentName": "Fig Temperature- pressure diagram showing the three major types of metamorphic facies series proposed by Miyashiro (1973, 1994). Winter (2001) An Introduction to Igneous and Metamorphic Petrology. Prentice Hall.", "Image ImageDescription": "The low P/T series is characteristic of high-heat-flow orogenic belts (Buchan or Ryoke- Abukuma type), rift areas, or contact metamorphism. The sequence of facies may be a low-pressure version of the medium P/T series described above (but with cordierite and/or andalusite), or the sequence (zeolite facies) - albite-epidote hornfels facies - hornblende hornfels facies - pyroxene hornfels facies. Sanidinite facies rocks are rare, requiring the transport of great heat to shallow levels.", "Image XResolution": "200", "Image YResolution": "200", "Image ResolutionUnit": "Pixels/Inch", "Image Software": "SlidePlayer", "Image YCbCrPositioning": "Centered"}