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Magnetic Properties of Rocks and Minerals

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TLDR
In this article, an updated collation of magnetic parameters of rocks and minerals for geologists, geochemists, and geophysicists is presented, and best-fit equations have been provided for some of the displayed ata so that interpolations can be made easily.
Abstract
This is an updated collation of magnetic parameters of rocks and minerals for geologists, geochemists, and geophysicists. Since the publication of the previous edition of Handbook of Physical Constants [74], two other collations have appeared [16, 18]. In addition, selected magnetic parameters have also been assembled [19, 22, 38, 41, 88]. Rather than produce a fully comprehensive collection, we have aimed for high-precision data obtained from wellcharacterized samples. Both tables and figures have been used for presenting the data, and best-fit equations have been provided for some of the displayed ata so that interpolations can be made easily. In an attempt to discourage the use of the outdated cgs system, all values are in the SI system (see Moskowitz, this volume). References have been cited for the sources used here. However, a more comprehensive bibliography has also been provided from which information can be extracted for samples which have not been included. The single-crystal constants and their variation with temperature and composition are for use by rock magnetists. Paleomagnetists and magnetic anomaly modelers have been provided with the magnetic properties of rocks and polycrystalline mineral samples. Lastly, we have made an effort to address the needs of environmental magnetism, a new group of researchers who require the values of sizeand

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Citations
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Journal ArticleDOI

Environmental magnetism: Principles and applications

TL;DR: In this article, a review of magnetic properties and the environmental processes that give rise to the measured magnetic signal is presented, and the power of environmental magnetism in enabling quantitative environmental interpretations is discussed.
Journal ArticleDOI

Selected room temperature magnetic parameters as a function of mineralogy, concentration and grain size

TL;DR: In this paper, a data set of room temperature magnetic parameters for several iron oxides and sulphides was compiled from the available literature, and the most effective methods for assessing mineralogy, concentration and domain state within environmental magnetic studies were proposed.
Journal ArticleDOI

Magnetic properties of sedimentary greigite (Fe3S4): An update

TL;DR: In this paper, the authors systematically document the known magnetic properties of greigite (at high, ambient, and low temperatures and with alternating and direct fields) and illustrate how grain size variations affect magnetic properties.
Journal ArticleDOI

An 85-ka record of climate change in lowland Central America

TL;DR: Drill cores obtained from Lake Peten Itza, Peten, Guatemala, contain a ∼85-kyr record of terrestrial climate from lowland Central America that was used to reconstruct hydrologic changes in the northern Neotropics during the last glaciation as discussed by the authors.
Journal ArticleDOI

Structural geology, petrofabrics and magnetic fabrics (AMS, AARM, AIRM)

TL;DR: Anisotropy of magnetic susceptibility (AMS) was recognized as a feature of minerals in 1899, and petrofabric-compatible AMS fabrics were reported from 1942-1958 as mentioned in this paper.
References
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Book

Introduction to Magnetic Materials

TL;DR: In this paper, the authors present materials at the practical rather than theoretical level, allowing for a physical, quantitative, measurement-based understanding of magnetism among readers, be they professional engineers or graduate-level students.
Journal ArticleDOI

Hysteresis properties of titanomagnetites: Grain-size and compositional dependence

TL;DR: In this article, the grain-size dependence of parameters with coercive force as high as 2,000 Oe in x = 0.6 titanomagnetite was found.
Journal ArticleDOI

Magnetic properties of some synthetic sub-micron magnetites

TL;DR: In this article, the grain size dependence of various mineral (rock) magnetic parameters has been determined, using a series of essentially pure, fine-grained (single domain, SD) and ultrafine-gained (superparamagnetic, SP) magnetites.
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