Chromitites in ophiolites: How, where, when, why? Part II. The crystallization of chromitites

JM González-Jiménez, WL Griffin, JA Proenza… - Lithos, 2014 - Elsevier
A review of previous work relevant to the formation of concentrations of chromite in
peridotites from ophiolitic (sl) sequences highlights some of the key problems in …

The deep structure of the Alps based on the CIFALPS seismic experiment: A synthesis

MG Malusà, S Guillot, L Zhao, A Paul… - Geochemistry …, 2021 - Wiley Online Library
Abstract The European Alps are the site where classic geologic concepts such as nappe
theory, continental subduction and slab breakoff have been first proposed. However, the …

Intraplate volcanism originating from upwelling hydrous mantle transition zone

J Yang, M Faccenda - Nature, 2020 - nature.com
Most magmatism occurring on Earth is conventionally attributed to passive mantle upwelling
at mid-ocean ridges, to slab devolatilization at subduction zones, or to mantle plumes …

Water distribution across the mantle transition zone and its implications for global material circulation

S Karato - Earth and Planetary Science Letters, 2011 - Elsevier
Various methods for inferring the water distribution in Earth's mantle are reviewed including
geochemical and geophysical methods. The geochemical approach using the water …

On the origin of the asthenosphere

S Karato - Earth and Planetary Science Letters, 2012 - Elsevier
Various models of the origin of the asthenosphere are reviewed based on the latest
observations on mineral physics of mechanical properties, melting relationships and the …

Electrical conductivity of mantle minerals: Role of water in conductivity anomalies

T Yoshino, T Katsura - Annual review of earth and planetary …, 2013 - annualreviews.org
The electrical conductivity of Earth's mantle has recently become an interesting topic across
diverse Earth science communities. Many electrical conductivity data of mantle phases have …

Deep mantle melting, global water circulation and its implications for the stability of the ocean mass

S Karato, B Karki, J Park - Progress in Earth and Planetary Science, 2020 - Springer
Oceans on Earth are present as a result of dynamic equilibrium between degassing and
regassing through the interaction with Earth's interior. We review mineral physics …

Pervasive low-velocity layer atop the 410-km discontinuity beneath the northwest Pacific subduction zone: Implications for rheology and geodynamics

G Han, J Li, G Guo, WD Mooney, S Karato… - Earth and Planetary …, 2021 - Elsevier
Regional triplication waveforms of five intermediate-depth events are modeled to
simultaneously obtain the compressional (P) and shear (SH) wave velocity structure …

Stability of the hydrous phases of Al-rich phase D and Al-rich phase H in deep subducted oceanic crust

X Liu, K N. Matsukage, Y Nishihara, T Suzuki… - American …, 2019 - degruyter.com
To understand the stability of hydrous phases in mafic oceanic crust under deep subduction
conditions, high-pressure and high-temperature experiments were conducted on two …

Electrical conductivity of enstatite as a function of water content: Implications for the electrical structure in the upper mantle

B Zhang, T Yoshino, X Wu, T Matsuzaki, S Shan… - Earth and Planetary …, 2012 - Elsevier
The electrical conductivity of Ca-free aluminous enstatite with various water contents has
been determined at a pressure of 3GPa in a Kawai-type multi-anvil apparatus. Impedance …