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Автор(ы):Miall A.D.
Издание:Springer, 2000 г., 633 стр., ISBN: 3-540-65790-8
Язык(и)Английский
Principles of sedimentary basin analysis / Принципы анализа осадочных бассейнов

Basin analysis is a process that requires the collection and integration of a wide variety of different types of data. Many review articles and books are available that deal with some of the individual specialized fields that together constitute basin analysis, such as stratigraphic methods, facies analysis, geophysical methods, sedimentation and tectonics, and sequence stratigraphy; but this is one of the few books that has attempted, now through three editions, to show how these different types of data and the varying types of analytical methodology used in basin analysis need to be brought together to tackle specific basin-analysis problems. The emphasis in this book continues to be on the traditional geological skills of observation, description and synthesis.  <...>

Издание 4
Автор(ы):Boggs S.
Издание:Pearson Prentice Hall, 2006 г., 675 стр., ISBN: 0-13-154728-3
Язык(и)Английский
Principles of sedimentology and stratigraphy / Основы седиментологии и стратиграфии

The roots of sedimentology and stratigraphy extend back to the 16th century; however, these disciplines are still growing and changing. Geologists continue to "fine tune" sedimentologic and stratigraphic concepts through a variety of research avenues and by using an array of increasingly sophisticated research tools. T he result is a continuous outpouring of fresh data and new ideas. In fact, it is becoming increasingly difficult to keep abreast of the flood of new information appearing in the geological literature. A glance through recent issues of a well-known sedimentology journal reveals important new papers on sedimentation and tectonics, depositional systems, carbonates, biosedimentology, diageneis, provenance, geochemistry, sediment transport and sedimentary structures, stratigraphic architecture, chronostratigraphy, numerical modeling, paleoclimatology, sequence stratigraphy, and basin analysis-to name but a few research areas. <...>

Издание 2
Автор(ы):Buforn E., Udias A.
Издание:Cambridge, 2018 г., 573 стр., ISBN: 978-1-107-13869-8
Язык(и)Английский
Principles of Seismology / Принципы сейсмологии

A second edition of this textbook, first published 17 years ago, is a wonderful opportunity to review its contents and improve its pedagogical orientation, in view of the many comments and interactions received, teaching experience, and experimental progress in seismology over the intervening years. Seismology is the science of earthquakes, which are both natural disasters profoundly affecting human lives, and a subject of study through application of the principles of the physical sciences.

ТематикаГеофизика
Автор(ы):Udias A.
Издание:Cambridge University Press, 1999 г., 488 стр., ISBN: 0-521-62434-7
Язык(и)Английский
Principles of Seismology / Принципы сейсмологии

This book is an introductory text on seismology intended for advanced undergraduates and graduate students. The book, which emphasizes fundamental concepts and basic mathematical developments, is intended to be ‘student-friendly’.

ТематикаГеофизика
Издание 3
Автор(ы):Kim H.Tan
Издание:Marcel Dekker Inc, New York, 1998 г., 556 стр., ISBN: 0-8247-0147-X
Язык(и)Английский
Principles of soil chemistry / Принципы химии почв

As soon as the second edition of Principles of Soil Chemistry appeared, it was sought after by many scholars, students, professionals, and scientists interested in the chemistry of soils. It was chosen as the textbook at the University of Georgia for teaching the senior-level undergraduate and graduate course in soil chemistry. It has been used as a textbook in soil chemistry at the University of California, Davis, and other universities in the United States. Because of its simple language and style, which avoid making problems more complex than needed without sacrificing scientific standards, the book is particularly appealing as a textbook in many universities overseas. The first edition of Principles of Soil Chemistry was translated in Indonesian and published by the University of Gadjah Mada Press, Yogyakarta, under the title Dasar-Dasar Kimia Tanah, which soon sold out and is out of press. I was invited to teach Soil Chemistry and Soil Genesis courses for a semester in 1996 at the University of Andalas, Padang, Sumatra, Indonesia, and in 1995 at the Universidad Nacional del Sur, Bahia Blanca, Argentina, where my first and then the second edition were adopted as the main textbook for these courses.

Автор(ы):Sharp Z.
Издание:Pearson Prentice Hall, New Jersey, 2007 г., 359 стр., ISBN: 0-13-009139-1
Язык(и)Английский
Principles of stable isotope geochemistry / Принципы геохимии стабильных изотопов

Principles of Stable Isotope Geochemistr is written as a textbook to accompany a one semester course in stable isotope geochemistry. The book is tailored to an upper division or graduate level. There are 13 chapters, each dealing with a specifc subtopic of the feld. Other than Chapters 1 ad 2-introduction and defnitions-most of the remaining chapters can be read without reliance on any preceding ones. Therefore, a course can be customized to the interests of the instructor. It is also hoped that the book will serve as a general reference volume for researchers in the feld.

Автор(ы):Brookfield M.E.
Издание:Blackwell, 2004 г., 351 стр., ISBN: 1-4051-1164-X
Язык(и)Английский
Principles of stratigraphy / Принципы стратиграфии

Stratigraphy is one of the most demanding, fundamental, and interesting of geologic disciplines. It tries to reconstruct history with a few basic principles, requires both careful observation and wide-ranging imagination, and involves many individually fascinating subdisciplines. Yet, as the quotation above shows, this is not how it appears to many people. Stratigraphy has a poor image because it is sometimes presented only as a way of classifying and organizing strata with “codes.”

Издание 3
Автор(ы):Nevin C.M
Издание:John Wiley & Sons INC, New York, 1942 г., 320 стр.
Язык(и)Английский
Principles of structural geology / Принципы структурной геологии

Structural geology may be defined as a study of the framework of the earth's crust and the causes that are distorting it. However, in its broader phases, structural geology deals with deformation of the entire earth and is not limited merely to the crust. Although we see only a thin rind and although information about the greater bulk of the earth, the unseen vast interior, must of necessity be based on indirect evidence— yet it is to deep-seated adjustments that many of the surface crumplings arc attributed. The central theme of structural geology, then, is the deformation of the earth, its causes and effects. Unerring interpretation of observed rock structures is the goal sought.

At the outset, any idea of immobility of the earth should be dismissed from our minds. The crust oscillates to the rise and fall of the tides. Continual shifting of enormous sedimentary loads through the agencies of erosion, transportation, and deposition is attended by both deep-seated and surface adjustments. The shape of the earth itself is largely a response to the rate of axial spinning; modify the speed of rotation, and a corresponding change in the earth's shape, with attendant deformation of the crust, would inevitably follow. In short, the earth is not inert but is ceaselessly changing, and complete rigidity has no place in structural geology.

Beginning students of geology soon realize that the earth's crust has failed many times and in many places. Mountains of folded rock have been pushed up thousands of feet; enormous areas of relatively undisturbed formations have been gently tilted; beds once forming below ocean level have been raised several miles above their place of origin. All these and a host of other examples present a clear picture of tremendous masses moved great distances. The total forces involved in these distortions must have been stupendous, and we arc prone to think that this is all of the distant past — surely no major deformation of the earth is going on today or we should be able to see and measure it.

Indeed, there seems to be a rather general assumption that the earth is now passing through a stage of relative quiet, resting, as it were, after widespread recent deformations. Thus, the present is considered by many to be a poor key with which to unlock the structural mysteries of the past. <...>

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