Key Laboratory of High-Temperature and High-Pressure Study of the
Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences,
Guiyang, 550081, China
Wenqing Sun
Key Laboratory of High-Temperature and High-Pressure Study of the
Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences,
Guiyang, 550081, China
University of Chinese Academy of Sciences, Beijing, 100049, China
Heping Li
Key Laboratory of High-Temperature and High-Pressure Study of the
Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences,
Guiyang, 550081, China
Haiying Hu
Key Laboratory of High-Temperature and High-Pressure Study of the
Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences,
Guiyang, 550081, China
Lei Wu
Key Laboratory of High-Temperature and High-Pressure Study of the
Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences,
Guiyang, 550081, China
Jianjun Jiang
Key Laboratory of High-Temperature and High-Pressure Study of the
Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences,
Guiyang, 550081, China
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The gneiss conductivities markedly increase with total alkali and calcium ion content. The influence of pressure on gneiss conductivity is weaker than temperature, although conductivity still increases with pressure. The results cannot be used to interpret the HC anomalies in the Dabie–Sulu UHPM belt. However, the conductivity–depth profiles for gneiss may provide an important constraint on the interpretation of field magnetotelluric conductivity results in the regional metamorphic belt.
The gneiss conductivities markedly increase with total alkali and calcium ion content. The...