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- W1984767244 abstract "In the Gulf of Mexico, up to 11 km of sediments overlie a clearly oceanic crust. As much of the sediment appears to be of shallow-water origin, the question arises how it could be deposited to such thickness. A phase transition at a depth of 50–90 km could resolve the puzzle. A seismic discontinuity observed at 57 km is tentatively identified with this phase transition." @default.
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- W1984767244 date "1973-12-01" @default.
- W1984767244 modified "2023-09-27" @default.
- W1984767244 title "The crust of the Gulf of Mexico: A discussion" @default.
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- W1984767244 doi "https://doi.org/10.1016/0040-1951(73)90110-8" @default.
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