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Titlebook: Rock and Mineral Magnetism; W. O’Reilly Book 1984 Blackie & Son Ltd 1984 Pet.climatology.earth.evolution.fields.geophysics.hydrology.hyste

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發(fā)表于 2025-3-21 19:14:53 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Rock and Mineral Magnetism
編輯W. O’Reilly
視頻videohttp://file.papertrans.cn/832/831438/831438.mp4
圖書封面Titlebook: Rock and Mineral Magnetism;  W. O’Reilly Book 1984 Blackie & Son Ltd 1984 Pet.climatology.earth.evolution.fields.geophysics.hydrology.hyste
描述The past two decades have witnessed a revolution in the earth sciences. The quantitative, instrument-based measurements and physical models of. geophysics, together with advances in technology, have radically transformed the way in which the Earth, and especially its crust, is described. The study of the magnetism of the rocks of the Earth‘s crust has played a major part in this transformation. Rocks, or more specifically their constituent magnetic minerals, can be regarded as a measuring instrument provided by nature, which can be employed in the service of the earth sciences. Thus magnetic minerals are a recording magnetometer; a goniometer or protractor, recording the directions of flows, fields and forces; a clock; a recording thermometer; a position recorder; astrain gauge; an instrument for geo- logical surveying; a tracer in climatology and hydrology; a tool in petrology. No instrument is linear, or free from noise and systematic errors, and the performance of nature‘s instrument must be assessed and certified. This has been the task of the research worker in rock and mineral magnetism.
出版日期Book 1984
關鍵詞Pet; climatology; earth; evolution; fields; geophysics; hydrology; hysteresis; magnetism; magnetization; miner
版次1
doihttps://doi.org/10.1007/978-1-4684-8468-7
isbn_softcover978-1-4684-8470-0
isbn_ebook978-1-4684-8468-7
copyrightBlackie & Son Ltd 1984
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沙發(fā)
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https://doi.org/10.1007/978-1-4684-8468-7Pet; climatology; earth; evolution; fields; geophysics; hydrology; hysteresis; magnetism; magnetization; miner
地板
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Thermoremanent magnetization,ture, such as ulv?spinel. Although such minerals will not contribute to the natural remanent magnetization of rocks, they may acquire remanence in laboratory experiments aimed at understanding the processes believed to operate in nature, and the properties of the minerals themselves have intrinsic i
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Other remanence-inducing mechanisms,rals crystallizing in a solidifying magma above their Curie points and eventually acquiring TRM, an assemblage of grains produced during alteration at temperatures lower than their Curie point may become part-blocked isothermally at the alteration temperature by the CRM mechanism and, conceivably, p
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Magnetic properties of titanomagnetites and titanomaghemites,he crust of the Earth. Whereas some of the data has indeed been obtained from minerals, i.e. naturally occurring examples of the compounds of interest, much of our knowledge of the magnetic properties of the remanence carriers of rocks is based on laboratory-prepared synthetic analogues. We deal fir
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Book 1984ument is linear, or free from noise and systematic errors, and the performance of nature‘s instrument must be assessed and certified. This has been the task of the research worker in rock and mineral magnetism.
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