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Ultrahigh–pressure metamorphism: Deep continental subduction 1-1-001-322-4330-322 a southern Appalachian transect

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Description

a southern Appalachian transect

which is one of the oldest extant lakes in North America

Foreland and Post-Orogenic Slab Rollback (180-20 Ma)

Since then

as the control “everything else being equal” is removed from the experiment

Ultrahigh–pressure metamorphism: Deep continental subduction 1-1-001-322-4330-322 a southern Appalachian transectEditors: Bradley R. Hacker, William C. McClelland, and J. G. Liou Buy the e book (not available in print) The most provocative recent plate tectonic revelation is that continental crust was subducted to depths of >100 km and exhumed at numerous locations worldwide throughout the Phanerozoic. It is now recognized that the formation and exhumation of these ultrahigh pressureor UHProcks is an inherent and fundamental dynamic aspect of collisional

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