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....

Deskribapen osoa

Gorde:
Xehetasun bibliografikoak
Egile Nagusiak: Yining Zhang, Yanyao Zhang, Yun Liu, Xi Liu
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: MDPI AG 2019-03-01
Saila:Minerals
Gaiak:
cold slabs
crystallographic feature and structural evolution
first-principles simulation
mantle transition zone
metastable olivine wedge
metastable Fo-III wedge
thermodynamic properties
Sarrera elektronikoa:http://www.mdpi.com/2075-163X/9/3/186
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