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- W2008238442 abstract "Geomagnetic variation anomalies observed in the central part of Japan can be accounted for by highly conducting layers having a conductivity of 0.5 S/m or thereabouts beneath the Japan and Philippine seas. High temperature may be a possible cause of such layers if we take into account that temperature amounts to 1,000°C at a depth of 40 km beneath the areas of high heat flow in the Japan and Philippine seas. It seems difficult, however, to account for a conductivity of 0.5 S/m which is unusually high at a depth of 50 km or so by means of high temperature only. We can interpret such a high conductivity in terms of partial melting of peridotite in the upper mantle, provided highly conducting molten material is interconnected. This is in good agreement with the interpretation of low-velocity zones beneath the Japan and Philippine seas in terms of a partial melting of 4–6%." @default.
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- W2008238442 title "Partial melting and electrical conductivity anomalies beneath the Japan and Philippine seas" @default.
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- W2008238442 doi "https://doi.org/10.1016/0031-9201(75)90030-8" @default.
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