A Metastable Fo-III Wedge in Cold Slabs Subducted to the Lower Part of the Mantle Transition Zone: A Hypothesis Based on First-Principles Simulations

The metastable olivine (Ol) wedge hypothesis assumes that Ol may exist as a metastable phase at the P conditions of the mantle transition zone (MTZ) and even deeper regions due to inhibition of the phase transitions from Ol to wadsleyite and ringwoodite caused by low T in the cold subducting slabs....

Full description

Bibliographic Details
Main Authors: Yining Zhang, Yanyao Zhang, Yun Liu, Xi Liu
Format: Article
Language:English
Published: MDPI AG 2019-03-01
Series:Minerals
Subjects:
Online Access:http://www.mdpi.com/2075-163X/9/3/186