Petrology and age of Precambrian Aksu blueschist, NW China
Abstract
The first occurrence of blueschist in the Neoproterozoic signifies a transition in thermal regime from a warmer Archean–Proterozoic Earth to modern colder subduction characterized by blueschist facies or ultrahigh pressure metamorphism. To evaluate the thermal regime of the transition, we apply phase equilibrium modeling to the Aksu blueschist in northwestern China to constrain the pressure (P) and temperature (T) conditions of the peak mineral...
Paper Details
Title
Petrology and age of Precambrian Aksu blueschist, NW China
Published Date
Jun 1, 2019
Journal
Volume
326
Pages
295 - 311
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