Results 11 to 20 of about 1,324 (221)

Micromagnetic Tomography for Paleomagnetism and Rock-Magnetism. [PDF]

open access: yesJ Geophys Res Solid Earth, 2021
Abstract Our understanding of the past behavior of the geomagnetic field arises from magnetic signals stored in geological materials, e.g., (volcanic) rocks. Bulk rock samples, however, often contain magnetic grains that differ in chemistry, size, and shape; some of them record the Earth's magnetic field well, others are unreliable ...
de Groot LV   +9 more
europepmc   +10 more sources

The importance of clays in speleothem magnetic remanence acquisition [PDF]

open access: yesScientific Reports
Speleothems are promising recorders of paleosecular variation of the Earth’s magnetic field, but ambiguities remain about the physical processes active during remanence acquisition.
Rashida Doctor   +4 more
doaj   +2 more sources

Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in Soils

open access: yesFrontiers in Earth Science, 2021
Fires are an integral part of many terrestrial ecosystems and have a strong impact on soil properties. While reports of topsoil magnetic enhancement after fires vary widely, recent evidence suggests that plant ashes provide the most significant source of
Jessica L. Till   +3 more
doaj   +1 more source

Late Paleozoic Depositional Environments and Sediment Transport Directions of the Itararé Group Rocks From the State of São Paulo, Brazil, Determined From Rock Magnetism and Magnetic Anisotropy

open access: yesEarth and Space Science, 2021
Sedimentary rocks of the Itararé Group, deposited during the Late Paleozoic Ice Age in the Paraná Basin of South America, were collected throughout the state of São Paulo, Brazil, for an anisotropy of magnetic susceptibility (AMS) and rock‐magnetic study.
Dario Bilardello
doaj   +1 more source

High-Resolution Environmental Magnetism Using the Quantum Diamond Microscope (QDM): Application to a Tropical Speleothem

open access: yesFrontiers in Earth Science, 2021
Quantum diamond microscope (QDM) magnetic field imaging is a recently developed technique capable of mapping magnetic field sources in geologic samples at 1 micrometer resolution.
Roger R. Fu   +10 more
doaj   +1 more source

Single Particle Multipole Expansions From Micromagnetic Tomography

open access: yesGeochemistry, Geophysics, Geosystems, 2021
Micromagnetic tomography aims at reconstructing large numbers of individual magnetizations of magnetic particles from combining high‐resolution magnetic scanning techniques with micro X‐ray computed tomography (microCT).
David Cortés‐Ortuño   +2 more
doaj   +1 more source

Magnetic Mineralogy of Speleothems From Tropical-Subtropical Sites of South America

open access: yesFrontiers in Earth Science, 2021
Fe-bearing minerals are a tiny fraction of the composition of speleothems. They have their origin in the karst system or are transported from the drainage basin into the cave.
Plinio Jaqueto   +8 more
doaj   +1 more source

A First‐Order Statistical Exploration of the Mathematical Limits of Micromagnetic Tomography

open access: yesGeochemistry, Geophysics, Geosystems, 2022
The recently developed Micromagnetic Tomography (MMT) technique combines advances in high resolution scanning magnetometry and micro X‐ray computed tomography.
Frenk Out   +4 more
doaj   +1 more source

The Early Miocene Provenance Shift of ODP Site 1177 and Implications for the Tectonic Evolution of the Shikoku Basin, Philippine Sea Plate

open access: yesFrontiers in Earth Science, 2022
The Ocean Drilling Program Site 1177 recovered the oldest (∼23 Ma) sedimentary records in the Shikoku Basin, northeastern part of the Philippine Sea Plate.
Wei Liu   +10 more
doaj   +1 more source

Simulation of Natural Iron Oxide Alteration in Soil: Conversion of Synthetic Ferrihydrite to Hematite Without Artificial Dopants, Observed With Magnetic Methods

open access: yesGeochemistry, Geophysics, Geosystems, 2020
We present new results on the conversion of pure, undoped synthetic ferrihydrite, wet‐annealed at pH 6.56 and 90°C without stabilizing ligands, to nanophase goethite, hematite, and an intermediate magnetic phase, nanophase maghemite.
Dario Bilardello   +4 more
doaj   +1 more source

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