Abstract
Displaced benthic Foraminifera in semiconsolidated clayey sandstone from the Gorda Rise provide evidence for uplift of the deep-sea floor. The sediment was deposited by turbidity currents on the floor of the Escanaba Trough (the axial valley of the Gorda Rise) from a sublittoral source on the continental margin to the east....
Recommended Citation
Fowler, Gerald A., and L. D. Kulm. 1970. "Foraminiferal and sedimentological evidence far uplift of the deep-sea floor, Gorda Rise, northeastern Pacific." Journal of Marine Research 28, (3). https://elischolar.library.yale.edu/journal_of_marine_research/1190
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