Effect of temperature, pressure and chemical composition on the electrical conductivity of granulite and geophysical implications
Author:
Affiliation:
1. University of Chinese Academy of Sciences
2. Key Laboratory of High–Temperature and High–Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/114/2/114_181107b/_pdf
Reference49 articles.
1. Behera, L. (2011) Crustal tomographic imaging and geodynamic implications toward south of Southern Granulite Terrain (SGT), India. Earth and Planetary Science Letters, 309, 166–178.
2. Bhowmik, S.K., Dasgupta, S., Baruah, S. and Kalita, D. (2018) Thermal history of a Late Mesoproterozoic paired metamorphic belt (?) during Rodinia assembly: New insight from medium–pressure granulites from the Aravalli–Delhi Mobile Belt, Northwestern India. Geoscience Frontiers, 9, 335–354.
3. Chen, S.B., Guo, X.Z., Yoshino, T., Jin, Z.M. and Li, P. (2018) Dehydration of phengite inferred by electrical conductivity measurements: Implication for the high conductivity anomalies relevant to the subduction zones. Geology, 46, 11–14.
4. Collins, A.S., Clark, C. and Plavsa, D. (2014) Peninsular India in Gondwana: The tectonothermal evolution of the Southern Granulite Terrain and its Gondwanan counterparts. Gondwana Research, 25, 190–203.
5. Dai, L.D., Li, H.P., Hu, H.Y. and Shan, S.M. (2009) Novel technique to control oxygen fugacity during high–pressure measurements of grain boundary conductivities of rocks. Review of Scientific Instruments, 80, 033903, https://doi.org/10.1063/1.3097882.
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