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Издание 10
Автор(ы):Levin H.
Издание:Wiley, 2013 г., 623 стр., ISBN: 978-1-118-25467-7
Язык(и)Английский
The Earth through time / Земля сквозь время

Students enrol in an Earth History course for many reasons. Often it is simply to satisfy a college science requirement. Those of us who teach the course, however, strive to provide a better reason. We hope to instill in our students knowledge about how our planet became a haven for life; how change has dominated Earth history; and how change will continue to challenge us in the future. In the geologic past, change has been driven by natural forces. Now we humans, only recently arrived on Earth, are an additional cause of change. More often than not, we cause change that is harmful. These are reasons why our students need to more fully understand this small and overcrowded planet. They need to learn from its history, its catastrophes, and its successes <...>

Издание 2
Автор(ы):Trewartha G.T.
Издание:The University of Wisconsin Press, 1981 г., 383 стр., ISBN: 0-299-08230-Х
Язык(и)Английский
The Earth's problem climates / Проблема изменения климата на Земле
Издание 2
Автор(ы):Korenaga J., Ozima M., Yin Q.-Z.
Издание:Cambridge University Press, 2012 г., 163 стр., ISBN: 978-0-521-76025-6
Язык(и)Английский
The Earth. Its birth and growth / Земля. Рождение и развитие

Recent environmental problems and natural disasters have given cause for increasing concern over the future habitability of our planet. It is becoming increasingly apparent that a clear understanding of the Earth's past evolution can provide the key to its possible future development. The Earth: Its Birth and Growth explores the evolution of the Earth over 4.6 billion years using basic reasoning and simple illustrations to help explain the underlying physical and chemical principles and major processes involved.

Издание:A Harcourt Science and Technology Company, 2000 г., 178 стр., ISBN: 0-12-158164-0
Язык(и)Английский
The Earth’s magnetism. A guided tour through magnetic fields / Земной магнетизм. Экскурсия сквозь магнитные поля

The year 2000 ushered in a major sunspot maximum period. Occurring every eleven years, spectacular sporadic solar outbursts of particles and fields bombard our Earth's space and continue at a high level for several years. In this time of majestic auroras and satellite-destroying magnetic storms, global interest focuses upon the curious Earth magnetism that guides the solar particles, with fields that penetrate our environment and affect our lives. <...>

Автор(ы):Lanza R., Meloni A.
Издание:Springer, 2006 г., 284 стр., ISBN: 978-3-540-27979-2
Язык(и)Английский
The Earth’s magnetism. An introduction for geologists / Земной магнетизм. Введение для геологов

Geomagnetism has always been at the forefront among the various branches of geophysics. At the end of the 16th century William Gilbert determined that the Earth is a big magnet, implying that it has a magnetic field; in the 1830s Carl Friedrich Gauss was able to formulate a procedure to measure the field completely and analyzed its characteristics with the spherical harmonic analysis, a method still used in the era of satellites and computers. Nevertheless, as recently as in the sixties, geophysics textbooks devoted only a thin chapter to geomagnetism, and limited their discussion mostly to prospecting methods, while many geologists’ curriculum practically left it out altogether. The essential contribution provided by the study of ocean floor magnetic anomalies and by paleomagnetism in the development of global tectonic models, made geomagnetism popular in the geological community, which nonetheless continued, and still continues, to view it as a highly specialist discipline. <...>

Автор(ы):Ghorbani M.
Издание:Springer, 2013 г., 580 стр., ISBN: 978-94-007-5624-3
Язык(и)Английский
The economic Geology of Iran. Mineral deposits and natural resources / Экономическая геология Ирана. Месторождения полезных ископаемых и минеральные ресурсы

 Iran is positioned on the southwest of Asia forming a bridge connecting three continents of Asia, Europe, and Africa. It is bordered by Azerbaijan, Armenia, Turkmenistan, and the Caspian Sea on the north, Afghanistan and Pakistan on the east, Oman Sea and Persian Gulf on the south, and Turkey and Iraq on the west (Road Atlas of Iran 2004 ) . The country is part of the Iranian Plateau that constitutes a vast and high terrane, which is bordered by the Caspian Sea on the north, Amu Darya, Syr Darya, and Kora River plains on the northeast, Sindh and Punjab Rivers plain on the southeast, the Oman Sea and the Persian Gulf on the south, and the Tigris river plain on the southwest (Comprehensive Geography of Iran 1987 ) <...>

Редактор(ы):Creti A.
Издание:Springer-Verlag, 2009 г., 122 стр., ISBN: 978-2-540-79406-6
Язык(и)Английский
The Economics of Natural Gas Storage. A European Perspective / Экономика хранения природного газа

Storage is indispensable to the operation of the gas sector, since consumption, which is strongly influenced by weather, is seasonal and supply is relatively inflexible. Storing gas thus helps to avoid oversized extraction and transportation infrastructures, as well as to limit excessive price fluctuations.

Seasonal gas storage allows to inject gas during the summer, when demand is low, and to withdraw it during the winter, when demand increases. Given this pattern, storage capacity is usually measured by the amount of working gas that can be used throughout the year.1 Storage also helps gas suppliers to face unpredictable demand fluctuations, including peak-days requirements exceeding the average winter consumption. Daily demand fluctuations can be dealt with storage inside pipelines, known as linepack and traditionally provided by the network operator. <...>

Редактор(ы):Kuangdi X.
Издание:Springer, 2024 г., 2428 стр., ISBN: 978-981-99-2085-3
Язык(и)Английский
The ECPH encyclopedia of mining and metallurgy / Энциклопедия горного дела и металлургии EC PH

Mining and metallurgical engineering encompasses two major disciplines: mining engineering and metallurgical engineering. Mining engineering separates useful minerals from worthless minerals (often called gangue) or harmful minerals through processes such as mining and mineral processing, or separates multiple useful minerals to obtain raw materials for metallurgy, energy, chemical industry, building materials, and other industries. Mining in a broad sense also includes the extraction of coal, oil, and gas, but this volume mainly focuses on the mining of metal ores. Metallurgical engineering applies the principle of metallurgy to smelt, process, and ultimately obtain metallic materials necessary for human society’s production and human life from the raw materials obtained in mineral engineering.

Автор(ы):Bas Den Brok
Издание:Journal of Structural Geology, 1996 г., 2 стр.
Язык(и)Английский
The effect of crystallographic orientation on pressure solution in quartzite

By measuring the degree of flattening and the orientation of the c-axis of single quartz grains in a naturally deformed ("cleaved") sandstone, Becker (1995) showed that: "quartz grains with a small angle between c-axis and the Z-axis of shortening exhibit the least amount of pressure solution, whereas grains with c-axes oriented at about 50° to Z manifest the highest degree of pressure solution". I briefly present some experimental results that show exactly the same. <...>

Выпуск 258
Автор(ы):Renner J., Rummel F.
Издание:Journal Tectonophysics, 1996 г., 19 стр.
Язык(и)Русский
The effect of experimental and microstructural parameters on the transition from brittle failure to cataclastic flow of carbonate rocks

Triaxial compression tests were conducted on cold-pressed calcite. aragonite and limestone aggregates and on Solnhofen limestone specimens to study the effect of experimental and microstructural parameters on the transition from brittle failure to cataclastic flow. The tests were performed at confining pressures up to 195 MPa and at strain rates between 5 • 10-4 s-1 and 5 • 10-6 s-1. Axial as well as volumetric strain were measured. Samples were produced by cold-pressing powders of crushed calcite and aragonite crystals and of crushed Solnhofen limestone. Sample porosity ranged between 5 and 25% and the average grain size varied between 5 and 400 µm.

For both the cold-pressed aggregates and the intact limestone specimens, the confining pressure at the transition from localized brittle failure to non-localized cataclastic flow decreases with increasing porosity and grain size. The transition is characterized by a zero work-hardening coefficient, by dilation for low porosity and compaction for high porosity rocks, by a constant ratio between axial stress and confining pressure, and by decreasing yield strength for increasing confining pressure. The experimental results disagree with the critical state concept over most of the porosity range investigated, and indicate non-associated material behaviour. These properties of the brittle-ductile transition are addressed on the basis of continuum mechanics or by models suggested for granular materials. The problems discussed and the results obtained are of fundamental interest to rock deformation and structural geology.


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