Добрый день, Коллеги. Важное сообщение, просьба принять участие. Музей Ферсмана ищет помощь для реставрационных работ в помещении. Подробности по ссылке

Поиск по книгам
Издание:CRC Press, 2023 г., 612 стр., ISBN: 978-0-367-71270-9
Язык(и)Английский
Thematic cartography and geovisualization / Тематическая картография и геовизуализация

We are pleased to offer this fourth edition of Thematic Cartography and Geovisualization published by CRC Press. We deem a fourth edition particularly appropriate given the extensive developments that have taken place in cartography and GIScience since the third edition was first published in 2009. One development is the continued evolution of the Internet and the associated World Wide Web, which is commonly referred to as Web 2.0. One characteristic of Web 2.0 is the ability to harness the collective intelligence of Web users. In the case of geography, we often refer to this collective intelligence as “volunteered geographic information” or VGI;

Редактор(ы):Stixrude L., Wentzcovitch R.
Издание:2010 г., 503 стр.
Язык(и)Английский
Theoretical and computational methods in mineral physics: Geophysical applications / Теоретические и вычислительные методы в физике полезных ископаемых: Геофизическое применение

Mineral physics is one of the three pillars of geophysics, the other two being geodynamics and seismology. Geophysics advances by close cooperation between these fields. As such, mineral physicists investigate properties of minerals that are needed to interpret seismic data or that are essential for geodynamic simulations. To be useful, mineral properties must be investigated in a wide range of pressures, temperatures, and chemical compositions.

Автор(ы):Tromp J.
Издание:Princeton University Press, 2025 г., 600 стр., ISBN: 9780691267968
Язык(и)Английский
Theoretical and computational seismology / Теоретическая и вычислительная сейсмология

This book presents over twenty-five years of research dedicated to the application of spectralelement and adjoint-state methods in seismology. If someone had told me, upon completing my PhD in 1992, that we would be able to simulate global seismic wave propagation in fully three-dimensional Earth models within ten years, I would have been skeptical.

Издание:Oxford university press, 1992 г., 528 стр., ISBN: 0-19-504403-7
Язык(и)Английский
Theoretical geochemistry: Applications of quantum mechanics in the Earth and mineral sciences / Теоретическая геохимия: применение квантовой механики в науках о Земле и минералах

Geochemistry is most obviously defined as the "study of the chemistry of the Earth." In the broadest sense, the subject attempts to describe and understand the distribution of the elements (and their isotopes) in all parts of the Earth; the atmosphere, and hydrosphere, the Earth's crust, and its deeper interior (mantle and core). However, geochemists have traditionally concentrated their attention on the solid Earth and on surface or near-surface processes involving fluids, leaving the atmosphere and hydrosphere to other specialists such as the atmospheric scientists and chemical oceanographers. Geochemists have also concerned themselves with the chemistry of extraterrestrial matter (strictly termed cosmochemistry) because of its importance in understanding the origin and history of the solar system and hence of the Earth. A recent, and very welcome, development is the growth of interdisciplinary fields (such as biogeochemistry) and a return to attempts to view the chemical systems of the Earth (lithosphere, hydrosphere, biosphere, and atmosphere) as a whole. <...>

Автор(ы):Monin A.S.
Издание:Kluwer Academic Publishers, 1988 г., 404 стр., ISBN: 978-94-010-7339-4
Язык(и)Английский
Theoretical geophysical fluid dynamics / Теоретическая геофизическая гидродинамика

Preferring to leave history to the historians of science, we will not present here a historical survey, but rather will only cite some examples of priorities during the course of the book. We will just note that separating geophysical fluid dynamics from general fluid dynamics was a risky step to take, since it could well have cut the field off from general science by creating a specialized jargon that was incomprehensible to the uninitiated. Pseudosciences can thrive and flourish on such soil over an area which is vast but which fails to reach any heights. This has occurred, for instance, in meteorology (here we do not include atmospheric physics), in which interest in astrological techniques for weather forecasting periodically rears its head (even now unverifiable forecasting methods 'for the season' are still used), in the agricultural sciences, in pedagogy, etc. However, things are quite different if, in an important sphere of knowledge, there is a solid nugget of seriousness, requiring a special study of the material and the creation of new concepts (the creation of new concepts goes deeper than just the recognition of patterns; it is the very basis of scientific creativity, distinguishing the investigator from the computers of the foreseeable future), and if, basing itself on these concepts, the new science contacts and interacts with other branches of knowledge and becomes generally used. <...>

Редактор(ы):Flemal R.C., Melhorn W.N.
Издание:George Allen & Unwin Ltd, London, 1975 г., 306 стр.
Язык(и)Английский
Theories of Landform Development / Теория развития рельефа

Theories of landscape development serve to stimulate communication between the interdependent descriptive, genetic-historical, and process-oriented lines of inquiry in geomorphology, and thereby help to unify them into one science. The theory that has dominated the modern era of geomorphology, which may be said to have begun in 1877 with the publication of G. K. Gilbert’s “Land Sculpture”, was first formulated by W. M. Davis in 1889 and 1899.

Издание 3
Редактор(ы):Pitard F.F.
Издание:CRC Press, 2019 г., 726 стр., ISBN: 9781138476486
Язык(и)Английский
Theory of sampling and sampling practice / Теория и практика опробования

Numerous articles and a few books have been written about sampling of particulate materials before this third edition. Then, why select Pierre Gy’s theory, Visman and Ingamells’s works? As a Pierre Gy’s Gold Medalist I want to bring my knowledge and experience on the Theory of Sampling (TOS) and contribute to making sure TOS grows in a rational way, in spite of its many detractors. Looking at comments made around the world, it is clear that many statisticians and empiricists promoting “Measurement of Uncertainty” (MU) strongly believe that TOS is something they can live without. Such antagonism is misplaced, unjustified and very unfair. I also strongly believe the MU promoters, who most of the time, are more comfortable with J. Visman’s work, need TOS, and vice versa. In this third edition of my book a special effort is made to integrate J. Visman and C. O. Ingamells’s works into the TOS and create a unified foundation that may help to create better sampling standards. <...>

Автор(ы):Anderson D.L.
Издание:Blackwell, 1989 г., 379 стр., ISBN: 0-86543-335-0
Язык(и)Английский
Theory of the Earth / Теория Земли

The maturing of the Earth sciences has led to a fragmentation into subdisciplines which speak imperfectly to one another. Some of these subdisciplines are field geology, petrology, mineralogy, geochemistry, geodesy and seismology, and these in turn are split into even finer units. The science has also expanded to include the planets and even the cosmos. The practitioners in each of these fields tend to view the Earth in a completely different way. Discoveries in one field diffuse only slowly into the consciousness of a specialist in another. In spite of the fact that there is only one Earth, there are probably more Theories of the Earth than there are of astronomy, particle physics or cell biology where there arc uncountable samples of each object. Even where there is cross-talk among disciplines, it is usually as noisy as static. Too often, one discipline’s unproven assumptions or dogmas are treated as firm boundary conditions for a theoretician in a slightly overlapping area. The data of each subdiscipline are usually consistent with a range of hypotheses. The possibilities can be narrowed considerably as more and more diverse data are brought to bear on a particular problem.

Редактор(ы):Mumpton F.A.
Издание:The Clay Minerals Society, 1990 г., 201 стр.
Язык(и)Английский
Thermal analysis an clay science / Термический анализ - наука о глине

Introduction R. F. Giese
Precision Scanning Calorimetry of Clay Minerals and their Intercalates R. F. Giese
High-Pressure Differential Thermal Analysis: Applications to Clay Minerals A. F. Koster van Groos and Stephen Guggenheim
Thermogravimetric Analysis of Minerals D. L. Bish and C. J. Duffy
Vacuum Thermogravimetric Analysis and Evolved Gas Analysis by Mass Spectrometry F. J. Wicks and R. A. Ramik
Mineral Index J. W. Stucki

Издание:PGS Publishing, Linden Park, 2005 г., 16 стр.
Язык(и)Английский
Thermal History Analysis of Selected Chilean, Indonesian and Iranian Porphyry Cu-Mo-Au Deposits / Анализ термической истории избранных медно-молибден-порфировых золоторудных месторождений Чили, Индонезии и Ирана

This paper presents U-Pb-He triple-dating age detenninations for several porphyry Cu±Mo+Au deposits in Chile, Indonesia and Iran in an effort to determine their thermal histories and to explore the effects of cooling/exhumation rates on ore formation and preservation processes. Inverse thermal modelling of measured time-temperature history data from these deposits was conducted to quantitatively constrain the depth of emplacement, duration of ore deposition, exposure ages and cooling/exhumation rates. The duration of hypogene ore formation for the deposits studied generally occurs within timeframes of 105 years, although modelling results for the Grasberg, Batu Hijau and El Teniente super porphyry deposits suggest formation periods of the order of 104 years. Emplacement depths on intrusions associated with porphyry mineralisation range from 800 m to 5500 m from the palaeosurface, with Grasberg and Rio Blanco being respectively the shallowest and deepest super porphyry deposits studied. The thermochronology data indicates a positive correlation between metal grade and cooling rate during hypogene ore formation, but further investigation is warranted. Exhumation rates varying from 0.3 to 1.1 km/m.y. have implications for the preservation potential of hypogene ore deposits, with super porphyry deposits like Sar Cheshmeh potentially losing 3.5 Mt of copper to erosion over the last 5 million years. The potential for supergene ore formation under such conditions is high, as is the potential for the formation of proximal Exotica-type deposits.

875.19