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Rock magnetism of sediments in the Angola-Namibia upwelling system with special reference to loss of magnetization after core recovery [PDF]
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Pre-existing structural control on the recent Holuhraun eruptions along the Bárðarbunga spreading center, Iceland. [PDF]
Døssing A +5 more
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Role of land-ocean interactions in stepwise Northern Hemisphere Glaciation. [PDF]
Zhong Y +22 more
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Updates on the Advantages and Disadvantages of Microscopic and Spectroscopic Characterization of Magnetotactic Bacteria for Biosensor Applications. [PDF]
Paul NL, Popa CO, Ionescu RE.
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The origins of light-independent magnetoreception in humans. [PDF]
Shibata T +4 more
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Detrital remanent magnetization: Viscosity theory of the lock‐in zone
Journal of Geophysical Research: Solid Earth, 1982Post‐depositional remanent magnetization (PDRM) becomes permanent within a lock‐in zone, whose apparent time delay (depth) and time span (thickness) are related to the characteristic time constants of compaction and magnetic grain rotation. Two simple models of the PDRM lock‐in zone are described, using Yaskawa's idea of effective sedimentary viscosity,
Charles R. Denham, Alan D. Chave
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Detrital remanent magnetization in hematite
Journal of Geophysical Research: Solid Earth, 1983Heavy mineral placer layers within channel sandstones of the Morrison Formation (western United States) have been shown to contain a very stable, accurate record of the Jurassic geomagnetic field. These laminae are composed almost entirely of hematite grains; in particular, they are largely the hematite pseudomorph of magnetite, martite.
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Earth and Planetary Science Letters, 1977
Abstract Deposition experiments have been carried out to measure the effect of particle size variation on the relationship between detrital remanent magnetization (DRM), anhysteretic remanent magnetization (ARM), and geomagnetic field intensity in sediments.
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Abstract Deposition experiments have been carried out to measure the effect of particle size variation on the relationship between detrital remanent magnetization (DRM), anhysteretic remanent magnetization (ARM), and geomagnetic field intensity in sediments.
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Journal of Geophysical Research: Solid Earth, 1983
Paleomagnetic studies of magnetite‐bearing lacustrine sediments from two late Pleistocene sections (age range about 12,000–23,000 14C years), one at Devlins Park in the Front Range, the other at Triangle Park in the northern end of the Sawatch Range, Colorado, indicate that detrital remanent magnetization of fine‐grained (silty clay) sediments at both ...
J. G. Rosenbaum, E. E. Larson
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Paleomagnetic studies of magnetite‐bearing lacustrine sediments from two late Pleistocene sections (age range about 12,000–23,000 14C years), one at Devlins Park in the Front Range, the other at Triangle Park in the northern end of the Sawatch Range, Colorado, indicate that detrital remanent magnetization of fine‐grained (silty clay) sediments at both ...
J. G. Rosenbaum, E. E. Larson
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