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Titlebook: Geomagnetism and Palaeomagnetism; F. J. Lowes,D. W. Collinson,A. Soward Book 1989 Kluwer Academic Publishers 1989 Catalog Service for the

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發(fā)表于 2025-3-21 16:28:43 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Geomagnetism and Palaeomagnetism
編輯F. J. Lowes,D. W. Collinson,A. Soward
視頻videohttp://file.papertrans.cn/384/383412/383412.mp4
叢書名稱Nato Science Series C:
圖書封面Titlebook: Geomagnetism and Palaeomagnetism;  F. J. Lowes,D. W. Collinson,A. Soward Book 1989 Kluwer Academic Publishers 1989 Catalog Service for the
描述This volume presents lectures given at the NATO Advanced Study Institute held 11-22 April 1988 at Newcastle upon Tyne, England. The aim of the Institute was to improve the interaction between workers in observational geomagnetism (using historical data) and archaeo- and palaeo-magnetism (using the remanent magnetization of man-made artefacts and of natural sediments and rocks) and those trying to interpret the data in terms of mechanisms inside or outside the Earth, particularly those developing dynamo theories of the field. The material discussed ranged from magnetic bacteria swimming round a circle in a few seconds, the effect of El Nino, through secular variation with time scales of tens to thousands of years and the‘mechanics of individual field reversals and excursions (aborted reversals?) to possible modulation of average reversal frequency on the hundred million year time scale. Many members of the Physics Department helped with the organization, and we are most grateful to them, and in particular to Anne Codling for her very many contributions. We also gratefully acknowledge the painstaking work of Aileen Dryburgh and Lynn Whiteford in so carefully typing the manuscript.
出版日期Book 1989
關(guān)鍵詞Catalog Service for the Web; environment; magnetic field; magnetism; modelling; sediment; solar system
版次1
doihttps://doi.org/10.1007/978-94-009-0905-2
isbn_softcover978-94-010-6896-3
isbn_ebook978-94-009-0905-2Series ISSN 1389-2185
issn_series 1389-2185
copyrightKluwer Academic Publishers 1989
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Geomagnetic Secular Variationl means of the vector magnetic field components measured at nearly one hundred magnetic observatories widely distributed about the Earth. The data that have been analyzed are for the time interval 1961–1977..Spherical harmonic models for each year within the indicated time interval have been compute
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Geomagnetic Secular Variation in Britain During the Last 2000 Yearstic implications of these observations. Older periods, although becoming defined, are not yet adequate for such analyses. Some smoothing of the younger data is still required, for which a 25 year window has been used. The data have also been corrected for spatial variation, at any given time, using
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The Lac Du Bouchet Palaeomagnetic Record: Its Reliability and Some Inferences about the Character of00 years. The first set, derived from six 9 m Mackereth cores covers the interval back to 38000 years BP. The second and third sets extend back to about 50000 years BP. They are derived respectively from six 12 m Mackereth cores and from five Livingston cores. Holocene data have been removed from th
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Developments in Cave Sediment Palaeomagnetism and negligible bioturbation. Consequently, the remanent magnetisation of these materials can yield high fidelity records of the geomagnetic field which spans a far longer timescale than is accessible by lake sediment coring. This paper describes sampling techniques developed for cave sediment palae
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