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- W2369969768 abstract "Magnetotelluric measurements were carried out in the Xingtai earthquake area to study earthquakes in connection with the conductivity structure in the area. The results indicate that the structure is complicated and the conductivity varies significantly among different locations. One-dimensional inversions give a 5-layer structure and the third layer at the depth from. 10 to 20 km is highly conductive. A considerable change in depth of the conductive layer appears as crossing the earthsuake region. The conductivity also varies laterally. Macroscopically, it is resistive in the earthquake region; but the earthquakes occurred at the location where the resistivity is rather low and its gradient is rather large." @default.
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- W2369969768 date "1990-01-01" @default.
- W2369969768 modified "2023-09-25" @default.
- W2369969768 title "MAGNETOTELLURIC STUDIES IN THE XINGTAI EARTHQUAKE AREA OF EASTERN CHINA" @default.
- W2369969768 hasPublicationYear "1990" @default.
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