Chapter 8: Major Elements - Faculty web pages
Chapter 8: Major Elements - Faculty web pages
Chapter 8: Major Elements - Faculty web pages
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Pressure-Temperature<br />
Temperature-Time Time (P-T-t) Paths<br />
<br />
Classic view: regional metamorphism is a result of deep<br />
burial or intrusion of hot magmas<br />
<br />
Plate tectonic view: regional metamorphism is a result of<br />
crustal thickening and heat input during orogeny at<br />
convergent plate boundaries (not simple burial)