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Titlebook: Origin of Thermoremanent Magnetization; Proceedings of AGU 1 David J. Dunlop Conference proceedings 1977 Center for Academic Publications J

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发表于 2025-3-21 17:34:28 | 显示全部楼层 |阅读模式
书目名称Origin of Thermoremanent Magnetization
副标题Proceedings of AGU 1
编辑David J. Dunlop
视频video
丛书名称Advances in Earth and Planetary Sciences
图书封面Titlebook: Origin of Thermoremanent Magnetization; Proceedings of AGU 1 David J. Dunlop Conference proceedings 1977 Center for Academic Publications J
描述Physical and chemical studies of the earth and planets along with their sur­ roundings are now developing very rapidly. As these studies are of essentially international character, many international conferences, symposia, seminars and workshops are held every year. To publish proceedings of these meetings is of course important for tracing development of various disciplines of earth and plane­ tary sciences though publishing is fast getting to be an expensive business. It is my pleasure to learn that the Center for Academic Publications Japan and the Japan Scientific Societies Press have agreed to undertake the publication of a series "Advances in Earth and Planetary Sciences" which should certainly become an important medium for conveying achievements of various meetings to the aca­ demic as well as non-academic scientific communities. It is planned to publish the series mostly on the basis of proceedings that appear in the Journal of Geomagnetism and Geoelectricity edited by the Society ‘Of Terrestrial Magnetism and Electricity of Japan, the Journal of Physics of the Earth by the Seismological SOCiety of Japan and the Volcanological Society of Japan, and the Geochemical Journal
出版日期Conference proceedings 1977
关键词carr; development; magnetism; ocean; oceanic; temperature; volcano
版次1
doihttps://doi.org/10.1007/978-94-010-1286-7
isbn_softcover978-94-010-1288-1
isbn_ebook978-94-010-1286-7
copyrightCenter for Academic Publications Japan 1977
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Domain Structure of Titanomagnetites and Its Variation with Temperature, less than —40°C in the central to more than 70°C in the marginal zones of the crystals was found by observing the variation of the domain structure with temperature. The effect is explained by the different degree of maghemitization. TRM production in fields of 35 Oe revealed that the direction of
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The Demagnetization Field of Multidomain Grains,simply to the shape of the grain, no theoretical study of . has previously been completed. It is shown in this paper that. monotonically increases with increase in remanence in multidomain grains. Although . can be approximated by a constant in the limit of small displacements of domain walls from t
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The Preparation, Characterization and Magnetic Properties of Synthetic Analogues of Some Carriers ostem prepared by oxidation of Fe.Mg.Ti.O.(0<δ<0.35). The following properties were determined: unit cell edge, Curie temperature, thermomagnetic behaviour, saturation magnetization, isothermal remanence and coercive force. The introduction of Al, Mg and vacancies into titanomagnetites reduces satura
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Reduction of Hematite to Magnetite under Natural and Laboratory Conditions,tite occurs when the experiment is perfomed in vacuum but not when it is performed in air 2) the reduction is arrested when the sample is heated in air before the vacuum run. In addition, we have found that the reduction is controlled by backstreaming vacuum pump oils, which buffer the atmosphere in
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Thermal Overprinting of Natural Remanent Magnetization and K/Ar Ages in Metamorphic Rocks,ingle geological unit. We trace the steps necessary to resolve and date such magnetic overprints in three studies of intensely metamorphosed rocks from the Grenville Province of the Canadian Precambrian Shield. First, it is shown that the various components may be associated with different rock-form
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