Sedimentary effects of interplay between the Kuroshio Extension and Pacific plate motion

R. D. Jacobi; D. E. Hayes

doi:10.1130/0016-7606(1989)101<0549:SEOIBT>2.3.CO;2

Sedimentary effects of interplay between the Kuroshio Extension and Pacific plate motion

R. D. Jacobi
, D. E. Hayes

Earth Sciences

SUNY Buffalo

Research output: Contribution to journal › Article › peer-review

4 Scopus citations

Abstract

Spatial relationships suggest that the zone of condensed sediment section and the adjacent sediment drifts are causally related to the Kuroshio Extension. The condensed section probably results from the partial insulation of the sea floor from the normal "pelagic rain' due to the high-energy portion of the Kuroshio and from the erosion of the sea floor by benthic storms associated with the Kuroshio. -from Authors

Original language	English
Pages (from-to)	549-560
Number of pages	12
Journal	Bulletin of the Geological Society of America
Volume	101
Issue number	4
DOIs	https://doi.org/10.1130/0016-7606(1989)101<0549:SEOIBT>2.3.CO;2
State	Published - 1989

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10.1130/0016-7606(1989)101<0549:SEOIBT>2.3.CO;2

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title = "Sedimentary effects of interplay between the Kuroshio Extension and Pacific plate motion",

abstract = "Spatial relationships suggest that the zone of condensed sediment section and the adjacent sediment drifts are causally related to the Kuroshio Extension. The condensed section probably results from the partial insulation of the sea floor from the normal {"}pelagic rain' due to the high-energy portion of the Kuroshio and from the erosion of the sea floor by benthic storms associated with the Kuroshio. -from Authors",

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AU - Jacobi, R. D.

AU - Hayes, D. E.

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N2 - Spatial relationships suggest that the zone of condensed sediment section and the adjacent sediment drifts are causally related to the Kuroshio Extension. The condensed section probably results from the partial insulation of the sea floor from the normal "pelagic rain' due to the high-energy portion of the Kuroshio and from the erosion of the sea floor by benthic storms associated with the Kuroshio. -from Authors

AB - Spatial relationships suggest that the zone of condensed sediment section and the adjacent sediment drifts are causally related to the Kuroshio Extension. The condensed section probably results from the partial insulation of the sea floor from the normal "pelagic rain' due to the high-energy portion of the Kuroshio and from the erosion of the sea floor by benthic storms associated with the Kuroshio. -from Authors

UR - https://www.scopus.com/pages/publications/84879888918

U2 - 10.1130/0016-7606(1989)101<0549:SEOIBT>2.3.CO;2

DO - 10.1130/0016-7606(1989)101<0549:SEOIBT>2.3.CO;2

M3 - Article

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EP - 560

JO - Bulletin of the Geological Society of America

JF - Bulletin of the Geological Society of America

IS - 4

ER -

Sedimentary effects of interplay between the Kuroshio Extension and Pacific plate motion

Abstract

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