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, Seong-Jae Doh

Research output: Contribution to journalArticle

356 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 languageEnglish
Pages (from-to)4361-4375
Number of pages15
JournalJournal of Geophysical Research
Volume97
Issue numberB4
Publication statusPublished - 1992 Jan 1

Fingerprint

Lithology
deep-sea sediment
lithology
Magnetism
magnetic property
Neogene
Magnetic properties
Sediments
sediments
Rocks
Pleistocene
rocks
magnetic properties
rock
sediment
plots
magnetism

ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)
  • Environmental Science(all)

Cite this

Rock magnetism of late Neogene and Pleistocene deep-sea sediments : relationship to sediment source, diagenetic processes, and sediment lithology. / Bloemendal, J.; King, J. W.; Hall, F. R.; Doh, Seong-Jae.

In: Journal of Geophysical Research, Vol. 97, No. B4, 01.01.1992, p. 4361-4375.

Research output: Contribution to journalArticle

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