Rock magnetism of late Neogene and Pleistocene deep-sea sediments: relationship to sediment source, diagenetic processes, and sediment lithology

J. Bloemendal; J. W. King; F. R. Hall; S. J. Doh

doi:10.1029/91JB03068

Rock magnetism of late Neogene and Pleistocene deep-sea sediments: relationship to sediment source, diagenetic processes, and sediment lithology

J. Bloemendal, J. W. King, F. R. Hall, S. J. Doh

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516 Citations (Scopus)

Abstract

Bivariate scatter plots are used to illustrate variations in selected rock magnetic properties of late Neogene and Pleistocene deep-sea sediments. Overall, correlations between sediment magnetic properties and gross lithology is poor, and factors such as the source and transport path of terrigenous sediment, together with the action of reductive diagenetic processes, are the major controls on the magnetic properties. -from Authors

Original language	English
Pages (from-to)	4361-4375
Number of pages	15
Journal	Journal of Geophysical Research: Oceans
Volume	97
Issue number	B4
DOIs	https://doi.org/10.1029/91JB03068
Publication status	Published - 1992

ASJC Scopus subject areas

Geophysics
Forestry
Oceanography
Aquatic Science
Ecology
Water Science and Technology
Soil Science
Geochemistry and Petrology
Earth-Surface Processes
Atmospheric Science
Earth and Planetary Sciences (miscellaneous)
Space and Planetary Science
Palaeontology

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10.1029/91JB03068

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title = "Rock magnetism of late Neogene and Pleistocene deep-sea sediments: relationship to sediment source, diagenetic processes, and sediment lithology",

abstract = "Bivariate scatter plots are used to illustrate variations in selected rock magnetic properties of late Neogene and Pleistocene deep-sea sediments. Overall, correlations between sediment magnetic properties and gross lithology is poor, and factors such as the source and transport path of terrigenous sediment, together with the action of reductive diagenetic processes, are the major controls on the magnetic properties. -from Authors",

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year = "1992",

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AU - Bloemendal, J.

AU - King, J. W.

AU - Hall, F. R.

AU - Doh, S. J.

PY - 1992

Y1 - 1992

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AB - Bivariate scatter plots are used to illustrate variations in selected rock magnetic properties of late Neogene and Pleistocene deep-sea sediments. Overall, correlations between sediment magnetic properties and gross lithology is poor, and factors such as the source and transport path of terrigenous sediment, together with the action of reductive diagenetic processes, are the major controls on the magnetic properties. -from Authors

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U2 - 10.1029/91JB03068

DO - 10.1029/91JB03068

M3 - Article

AN - SCOPUS:0026476459

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JO - Journal of Geophysical Research: Oceans

JF - Journal of Geophysical Research: Oceans

IS - B4

ER -

Rock magnetism of late Neogene and Pleistocene deep-sea sediments: relationship to sediment source, diagenetic processes, and sediment lithology

Abstract

ASJC Scopus subject areas

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