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- W968310438 abstract "Development of the upper and middle La Jolla Fan system is controlled by the regional California Borderland structural grain. This tectonic fabric produces three upper fan distributary paths. The position of La Jolla Canyon is controlled by the geometry of a buried hard-rock structure. The northern Newport Canyon channels contain seismically detectable vertical stacks of channel sand bodies. Sediment from northern feeders and the central La Jolla Canyon-Fan form three-dimensional wedges that interfinger at their distal ends. La Jolla Fan system contains an interleaved set of sediment wedges derived from multiple sources, woven around the regional structural fabric of uplifts and basins." @default.
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- W968310438 date "1985-01-01" @default.
- W968310438 modified "2023-09-23" @default.
- W968310438 title "La Jolla Fan, Pacific Ocean" @default.
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- W968310438 doi "https://doi.org/10.1007/978-1-4612-5114-9_11" @default.
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