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Автор(ы):Parfitt E.A., Wilson L.
Издание:Blackwell, 2007 г., 255 стр., ISBN: 978-0-63205-443-5
Язык(и)Английский
Fundamentals of physical volcanology / Основы физической вулканологии

Our knowledge of the physics of how volcanoes work has expanded enormously over the past 40 years, as have our methods of studying volcanic processes. In the late 1960s, George Walker conducted experiments into the fall-out of volcanic particles from eruption clouds by using stopwatches to time the fall of pieces of tephra dropped down a stairwell at Imperial College, London.

Автор(ы):Ganat T.A.-A.O.
Издание:Springer, Seri Iskender, 2020 г., 161 стр., ISBN: 978-3-030-28139-7
Язык(и)Английский
Fundamentals of Reservoir Rock Properties / Основы коллекторских свойств горных пород

In general, naturally occurring rocks are saturated with fluids, water, oil, or gas (Amyx et al. 1960). Any formation rock can produce oil, gas, and water which are considered as reservoir rock. A reservoir rock is a rock has an adequate permeability and porosity to permit fluids flow, to accumulate and to extract in viable volumes (Daniel and Lapedes 1978).

Normally, hydrocarbons exist in sandstones, carbonate, and shales formations and also are present in metamorphic and igneous rocks (basement rock). The principal reservoir rocks are sandstone and carbonate formations. Typically, the physical properties and the composition of the sandstone and carbonate reservoir rocks are varying (Cecil 1949). Therefore, known the physical properties of reservoir rocks, reservoir engineers can estimate the hydrocarbon reserve and identified the ultimate reservoir recovery and determine the best effective production that is economically viable under the existing condition <...>

Автор(ы):Bagdassarov N
Издание:Oxford university press, 2022 г., 572 стр., ISBN: 978-1-108-42210-9
Язык(и)Английский
Fundamentals of rock physics / Основы физики горных пород

Rock physics encompasses practically all aspects of solid- and fluid-state physics. This book provides a unified presentation of the underlying physical principles of rock physics, covering elements of mineral physics, petrology and rock mechanics. After a short introduction on rocks and minerals, the subsequent chapters cover rock density, porosity, stress and strain relationships, permeability, poroelasticity, acoustics, conductivity, polarizability, magnetism, thermal properties and natural radioactivity. Each chapter includes problem sets and focus boxes with in-depth explanations of the physical and mathematical aspects of underlying processes.

Автор(ы):Kay S.M.
Издание:Pearson Prentice Hall, 1993 г., 602 стр.
Язык(и)Английский
Fundamentals of statistical signal processing. Estimation theory / Основы статистической обработки сигналов. Теория оценки

Parameter estimation is a subject that is standard fare in the many books available on statistics. These books range from the highly theoretical expositions written by statisticians to the more practical treatments contributed by the many users of applied statistics. This text is an attempt to strike a balance between these two extremes. The particular audience we have in mind is the community involved in the design and implementation of signal processing algorithms. As such, the primary focus is on obtaining optimal estimation algorithms that may be implemented on a digital computer. The data sets are therefore assumed to be samples of a continuous-time waveform or a sequence of data points. The choice of topics reflects what we believe to be the important approaches to obtaining an optimal estimator and analyzing its performance. As a consequence, some of the deeper theoretical issues have been omitted with references given instead. <...>

Автор(ы):Fletcher R.C., Pollard D.D.
Издание:Cambridge University Press, 2005 г., 515 стр., ISBN: 978-0-521-83927-3
Язык(и)Английский
Fundamentals of structural geology / Основы структурной геологии

Fundamentals of Structural Geology provides a new framework for the investigation of geological structures by integrating field mapping and mechanical analysis. It emphasizes the observational data, modern mapping technology, principles of continuum mechanics, and the mathematical and computational skills, necessary to map, describe, model, and explain deformation in the Earth’s lithosphere quantitatively.

Автор(ы):Serra O.
Издание:Elsevier, 1986 г., 662 стр., ISBN: 0-444-42620-5
Язык(и)Английский
Fundamentals of well-log interpretation 2. The interpretation of logging data / Основы интерпретации данных каротажа скважин 2. Интерпретация данных каротажа

Our modern society has a constant need for raw materials and energy. An on-going effort in exploration and research is necessary, therefore, to discover and develop them. And, in this effort, it is better to appeal to geology than to rely on chance. Geology is by definition "the study of the planet Earth. It is concerned with the origin of the planet, the material and morphology of the Earth, and its history and the processes that acted (and act) upon it to affect its historic and present forms" (Glossary of Geology, 1980).

Автор(ы):Monroe J.S., Wicander R.
Издание:International Thomson Editores, 1999 г., 363 стр., ISBN: 970-686-024-X
Язык(и)Испанский
Fundamentos de geologia / Основы геологии
Автор(ы):Clack J.A.
Издание:Indiana University Press, 2012 г., 559 стр., ISBN: 978-0-253-00537-3
Язык(и)Английский
Gaining ground the origin and evolution of tetrapods / Набирающий обороты вопрос о происхождении и эволюции четвероногих

Approximately 380 million years ago, something strange and significant happened on Earth. That time is part of an interval of Earth’s history called the Devonian period by scientists such as geologists and paleontologists, but in more popular imagination, it is known as the Age of Fishes. The reason for this is that after about 200 million years of earlier evolution, the vertebrates—animals with backbones—had produced an explosion of fishlike animals that lived in the nearshore lagoons, river estuaries, and lakes of the time. The strange thing that happened from the middle to the later parts of the Devonian period is that some of these fishlike animals evolved limbs with digits—fingers and toes. Over the ensuing 350 million years, these tetrapods gradually evolved from their aquatic ancestry into walking terrestrial vertebrates. These have dominated the land ever since this initial explosive radiation allowed them to colonize and exploit the land and its opportunities. The tetrapods, with their limbs and fingers and toes, include ourselves as humans, so that this distant Devonian event is profoundly significant for humans as well as for the planet <...>

Выпуск 378
Автор(ы):Shimamoto T., Uehara S.
Издание:Journal Tectonophysics, 2004 г., 13 стр.
Язык(и)Английский
Gas permeability evolution of cataclasite and fault gouge in triaxial compression and implications for changes in fault-zone permeability structure through the earthquake cycle

We report the results of permeability measurements of fault gouge and tonalitic cataclasite from the fault zone of the Median Tectonic Line, Ohshika, central Japan, carried out during triaxial compression tests. The experiments revealed marked effects of deformation on the permeability of the specimens. Permeability of fault gouge decreases rapidly by about two orders of magnitude during initial loading and continues to decrease slowly during further inelastic deformation. The drop in permeability during initial loading is much smaller for cataclasite than for gouge, followed by abrupt increase upon failure, and the overall change in permeability correlates well with change in volumetric strain, i.e., initial, nearly elastic contraction followed by dilatancy upon the initiation of inelastic deformation towards specimen failure. If cemented cataclasite suffers deformation prior to or during an earthquake, a cataclasite zone may change into a conduit for fluid flow. Fault gouge zones, however, are unlikely to switch to very permeable zones upon the initiation of fault slip. Thus, overall permeability structure of a fault may change abruptly prior to or during earthquakes and during the interseismic period. Fault gouge and cataclasite have internal angles of friction of about 36j and 45j, respectively, as is typical for brittle rocks.

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