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- W2045248829 abstract "A surface-ship gravity survey was made over the eastern part of the Mendocino escarpment. Free-air and Bouguer gravity anomaly maps are presented and, also, three hypothetical crustal and subcrustal cross sections over the escarpment (using published refraction data for control). East of about 130°W the Mendocino escarpment is found to be an escarpment in the Mohorovicic discontinuity; north of the escarpment there appears to be a thick low-density upper mantle layer which is interpreted as being chemically different from that south of the escarpment. The escarpment appears to be a result of the juxtaposition of two different density mantles, the entire region being essentially in isostatic equilibrium. West of about 130°W the escarpment is relatively small, and the mantle densities on both sides of it appear to be nearly the same. The significance of the gravity data is considered in terms of previous interpretations of the region." @default.
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- W2045248829 date "1967-02-15" @default.
- W2045248829 modified "2023-09-27" @default.
- W2045248829 title "Gravity and structure of the eastern part of the Mendocino escarpment" @default.
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- W2045248829 doi "https://doi.org/10.1029/jz072i004p01233" @default.
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