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Role of land-ocean interactions in stepwise Northern Hemisphere Glaciation. [PDF]

open access: yesNat Commun
Zhong Y   +22 more
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The origins of light-independent magnetoreception in humans. [PDF]

open access: yesFront Hum Neurosci
Shibata T   +4 more
europepmc   +1 more source
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Detrital remanent magnetization: Viscosity theory of the lock‐in zone

Journal of Geophysical Research: Solid Earth, 1982
Post‐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
openaire   +1 more source

Detrital remanent magnetization in hematite

Journal of Geophysical Research: Solid Earth, 1983
Heavy 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.
openaire   +1 more source

Measurement of the effect of particle size variation on the detrital remanent magnetization to anhysteretic remanent magnetization ratio in some abyssal sediments

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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Paleomagnetism of two Late Pleistocene lake basins in Colorado: An evaluation of detrital remanent magnetization as a recorder of the geomagnetic field

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
openaire   +1 more source

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