Melting Inside the Tibetan Crust? Constraint From Electrical Conductivity of Peraluminous Granitic Melt

Magnetotelluric and seismological studies suggested the presence of partial melts in the middle to lower Himalaya‐Tibetan crust. However, the melt fractions inferred by previous work were based on presumed electrical conductivity of melts. We performed measurements on the electrical conductivity of...

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Veröffentlicht in:	Geophysical research letters 2018-05, Vol.45 (9), p.3906-3913
Hauptverfasser:	Guo, Xuan, Zhang, Li, Su, Xue, Mao, Zhu, Gao, Xiao‐Ying, Yang, Xiaozhi, Ni, Huaiwei
Format:	Artikel
Sprache:	eng
Schlagworte:	Anisotropy Anomalies Composition Conductivity Data Electrical conductivity Electrical resistivity Fluids Geographical variations Geophysics Himalaya‐Tibet melting Melts peraluminous melt Seismic velocities Seismology
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