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- W2019793879 abstract "Geomagnetic variations recorded on the deep sea floor of the North-west Atlantic basin have been combined with simultaneous data recorded at nearby land stations to deduce the electrical resistivity structure to depths of several hundred kilometres. Over a period interval between about 30 min and one day, vertical gradients of the geomagnetic field variations are simply interpreted as induction from a plane two-layer structure with resistivity of about 7−20 Ω m in the upper 100 km, increasing to > 20 Ω m below. The lack of suitable high-frequency data precluded resolution of structures within the upper 30−50 km. The resistivity value implied for depths below 100 km is comparable to that deduced from similar studies in the Pacific Ocean basin." @default.
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- W2019793879 date "1976-11-01" @default.
- W2019793879 modified "2023-09-25" @default.
- W2019793879 title "Electrical resistivity structure beneath the North-west Atlantic Ocean" @default.
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- W2019793879 doi "https://doi.org/10.1111/j.1365-246x.1976.tb01276.x" @default.
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