The electrical conductivity of aqueous fluids containing 0.01, 0.1, and 1 M NaCl was
measured in a piston‐cylinder apparatus up to 900° C and 5 GPa. The conductivity …

Aqueous fluids are extensively present in the middle to lower crust, as revealed by seismic
and magnetotelluric soundings. The α− β quartz phase transition significantly affects many …

Aqueous fluids are regarded as the crucial origin of high conductivity and low velocity
anomalies observed by magnetotelluric and seismic surveys in the middle to lower …

Electrical conductivities of the clinopyroxene (Cpx)‐NaCl‐H2O system with various salinities
(5, 10, 15, 20, 25 wt%) and fluid fractions (5, 10, 15, 20, 25 vol%) were measured at 1 GPa …

The dehydration of hydrous minerals is one of the causes of high‐conductivity anomalies in
subduction zones. To determine the origin of these anomalies, the trade‐off between the …

Ilmenite is a common metallic oxide distributed in the mafic rocks from the Earth's upper
mantle, and thus the effect of ilmenite contents on the electrical structures of the Earth's …

The dehydration of clinochlore may supply water for the creation of high‐conductivity
anomalies and melting beneath volcanic arc. However, this process has not yet been …

The electrical conductivities of hydrous olivine (Ol) aggregates and Ol–H2O, Ol–NaCl–H2O
(salinity: 1–21 wt%; fluid fraction: 5.1–20.7 vol%), Ol–KCl–H2O (salinity: 5 wt%; fluid fraction …

Abstract Interpretation of deep earth structures from electromagnetic data requires the
constraint from the electrical conductivity of various minerals experimentally measured at …

Antigorite–olivine aggregates were synthesized to serve as representative lithologies of
subduction zones, which often suffered serpentinization due to the hydration of the mantle …