Define paleomagnetic dating

Title notes No physical items for this record Paleomagnetism is the study of the fossil magnetism in rocks.
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It has been paramount in determining that the continue reading have drifted over the surface of the Earth throughout geological time. The fossil magnetism preserved in the ocean floor has demonstrated how continental drift takes place through the process of sea-floor spreading. The methods and techniques used in paleomagnetic studies of continental rocks and of the ocean floor are described and then applied to determining horizontal movements of the Earth's crust over geological time. An up-to-date review of global paleomagnetic data enables million years of Earth history to be summarized in terms of the drift of the major crustal blocks over the surface of the Earth. The first edition of McElhinny's book was heralded define paleomagnetic dating a "classic and definitive text.
In the 25 years since the highly successful first edition of Palaeomagnetism and Plate Tectonics Cambridge, the many advances in the concepts, methodology, and insights into paleomagnetism warrant this new treatment. This completely updated and revised edition of Paleomagnetism: Continents and Oceans will be a define paleomagnetic dating resource for a broad audience of earth scientists as well as laypeople curious about magnetism, paleogeography, geology, and plate tectonics.
Because the book is intended for a wide audience of geologists, geophysicists, and oceanographers, it balances the mathematical and descriptive aspects of each topic. Geomagnetism and Paleomagnetism.

Main Features of the Geomagnetic Field. Origin of the Main Field. Variations of the Dipole Field with Time. Early Work in Paleomagnetism. Magnetism in Rocks. Geocentric Axial Dipole Hypothesis. Paleointensity Over Geological Times. Paleosecular Variation.

Rock Magnetism. Basic Principles of Magnetism. Magnetic Fields, Remanent and Induced Magnetism. Diamagnetism and Paramagnetism. Ferro- Antiferro- and Ferrimagnetism. Magnetic Minerals in Rocks. Iron Sulfides and Oxyhydroxides.
Physical Theory of Rock Magnetism. Magnetic Domains. Theory for Single Domain Grains. Magnetic Viscosity.]

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Description Summary: A MATLAB software tool has been developed to provide an easy to use graphical interface for the plotting and interpretation of paleomagnetic data. The tool takes either paleomagnetic directions or paleopoles and compares them to a user defined apparent polar wander path or secular variation curve to determine the age of a paleomagnetic sample. Ages can be determined in two ways, either by translating the data onto the reference curve, or by rotating it about a set location e. The results are then compiled in data tables which can be exported as an excel file. This data can also be plotted using variety of built-in stereographic projections, which can then be exported as an image file. This software was used to date the giant Sukhoi Log gold deposit in Russia. Sukhoi Log has undergone a complicated history of faulting, folding, metamorphism, and is the vicinity of many granitic bodies. Paleomagnetic analysis of Sukhoi Log allowed for the timing of large scale thermal or chemical events to be determined. Paleomagnetic analysis from gold mineralized black shales was used to define the natural remanent magnetization recorded at Sukhoi Log.![[BKEYWORD-0-3] Define paleomagnetic dating](http://eos.tufts.edu/varves/images/pmag_inc_05012006_large.jpg)
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