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Издание:Tucson, 2022 г., 744 стр., ISBN: 978-0-8165-4358-8
Язык(и)Русский
Mineralogy of Arizona / Минералогия Аризоны

Many new mineral species have been documented in Arizona since the third edition of Mineralogy of Arizona was published in 1995. This new edition adds to the extensive work of the previous authors, who built the foundation on which this new effort rests. This edition is dedicated to these men: John Anthony, Sidney Williams, and Richard Bideaux.The field of mineralogy has undergone many changes since the third edition.

Автор(ы):Whitfield R.P.
Издание:Goverment Printing Office, Washington, 1894 г., 193 стр.
Язык(и)Русский
Mollusca and crustacea of the miocene formations of New Jersey / Моллюски и ракообразные миоценовых образований Нью-Джерси

The fossils of the Miocene beds of New Jersey, like those of the Cretaceous and Eocene beds, have never until now been systematically studied or recorded. Many of them which are as yet peculiar to the deposits of the State have, however, been described haphazard, as it were, by different writers, with scarcely any other object in view than that of describing the species which happened to fall into their hands. In this way a few of the most prominent forms have become known, but very few species are mentioned in any of.the lists of Miocene fossils as pertaining to the New Jersey fauna.

Редактор(ы):DePaolo D.J.
Издание:The National Academies Press, 2008 г., 150 стр., ISBN: 0-309-11718-6
Язык(и)Русский
Origin and evolution of Earth / Происхождение и эволюция Земли

Over the past four decades, Earth scientists have made great strides in understanding our planet’s workings and history. We understand as never before how plate tectonics shapes our planet’s surface, how life can be sustained over billions of years, and how geological, biological, atmospheric, and oceanic processes interact to produce climate—and climatic change. Yet at the most basic level, this progress has served principally to lay bare more fundamental questions about Earth.

Издание:Пермь, 2013 г., 35 стр.
Язык(и)Русский
Permian period. Пермский период: местонахождения, флора и фауна

В неглубоких водоемах пермского периода привольно себя чувствовали дискозавриски - интересные существа, сочетавшие в своем строении признаки амфибий и рептилий. По современной систематике (Иванов, Черепанов, 2004) дискозавриски относятся к отряду антракозавров, подклассу батрахозавров («лягушкоящеров»), классу амфибий. Охотились дискозавриски, по всей видимости, на мелких личинок насекомых, различных водных беспозвоночных и рыбок.
Ископаемые остатки представителей семейства
дискозаврисцид найдены и в Приуралье, в Оренбургской области и в Куединском районе Пермского края, в местонахождении Куединекие Ключики. <...>

Автор(ы):Ghazban F.
Издание:2007 г., 733 стр., ISBN: 964-03-9420-3
Язык(и)Русский
Petroleum geology of the Persian gulf / Нефтяная геология Персидского залива

The intention of this book is to provide a detailed synthesis of the available information published on the petroleum geology of the Persian Gulf. Despite the intensive petroleum exploration which has taken place in the Persian Gulf over the past seventy years, relatively little has been published in the petroleum geology literature. One of the main reasons for this is that many of the studies are undertaken either for or by oil companies, who, for competitive reasons, impose restrictions on publication to maintain confidentiality. This information will aid in estimating oil and gas reserves as well as improving field development technology. Much work remains to be done regarding the geology of the Persian Gull. The need for a book on the geology of the Persian Gulf is therefore clear, and it is hoped that it will continue to provide a useful reference manual and resource of ideas for students as well as professionals. <...>

Издание 2
Автор(ы):Heiskanen W.A., Moritz H.
Издание:Institute of Physical Geodesy, Graz, 1993 г., 364 стр.
Язык(и)Русский
Physical Geodesy / Физическая геодезия

Almost every geodetic measurement depends in a fundamental way on the earth’s gravity field. Therefore, the study of the physical properties of the gravity field and their geodetic application, which are the subject of physical geodesy, forms an essential part of the geodesist’s education. During the ten years that have passed since the writing of The Earth and Its Gravity Field by Heiskanen and Vening Meinesz, geodesy has progressed enormously. To incorporate the results of this progress, which has been theoretical as well as practical, in a new edition of that book became increasingly impossible. It was necessary to write an entirely new textbook, one that is different in both scope and treatment. The great increase in the amount of available information required a strict limitation to geodetic aspects; advances in theory made neccssary an increased emphasis on mathematical methods. The outcome is the present book, which is intended to be theoretical in the sense in which the word is used in the term “theoretical physics.” This textbook, intended for graduate students, presupposes the background in mathematics and physics required by geodesy departments of American and European Universities. The necessary fundamentals of potential theory are presented in an introductory chapter. Chapters 1 through 5 cover the material for a basic course in physical geodesy. Chapters 6 through 8 present a number of more specialized and advanced topics, where current research activity is high. (These chapters are likely to be more subjectively biased than the others.) The reader who has mastered them should be able to begin research of his own. For the sake of completeness we have added a chapter on celestial methods; this material may be included in the basic course. We have tried hard to make the book sclf-contained. Detailed derivations are given wherever feasible. Our approach is intuitive: verba! explanations of the principles were felt to be more important than formal mathematical rigor, although the latter is not ignored. Our general attitude is conservative. We do not believe that the concept of the geoid has become obsolete. This docs not mean, however, that we are unaware of the great significance of recent theoretical developments associated mainly with the name of Molodensky: we discuss them in Chapter 8. Observational techniques such as those used in gravity measurements or astronomical observations are deliberately omitted as being out of place in a theoretically oriented presentation. Bibliographies of works cited in the text, many of which should be useful for further study, will be found at the end of each chapter; citation in the text is by author’s name and year of publication—for example, Kellogg (1929). We have not attempted to settle questions of priority. Names associated with formulas should be considered primarily as convenient labels. Similarly, the most readily accessible or most comprehensive publication of an author on a particular topic is given rather than his first. Most of our own research incorporated in this book has been done at The Ohio State University. We wish to thank Dr. Waiter D. Lambert for carefully checking parts of the manuscript for correct English.



Редактор(ы):Lehtinen M., Nurmi P.A., Ramo O.T.
Издание:Elsevier, 2005 г., 750 стр., ISBN: 978-0-444-51421-9
Язык(и)Русский
Precambrian geology of Finland key to the evolution of the fennoscandian shield / Геология докембрия Финляндии - ключ к эволюции фенноскандинавского щита

The Fennoscandian (or Baltic) Shield represents the largest outcropping domain of Precambrian bedrock in Europe, covering more than a million km2 throughout Norway, Sweden, Finland, and northwestern Russia. This book focuses on Finland, which occupies the central part of the shield and which, since the advent of modern geology in the 19th century, has been instrumental in a number of fundamental insights and advances in understanding Earth processes.

Выпуск 280
Автор(ы):Gratier J.P, Ortoleva P., Renard F.
Издание:Journal Tectonophysics, 1997 г., 10 стр.
Язык(и)Русский
Pressure solution in sandstones: influence of clays and dependence on temperature and stress

The enhancement of dissolution of quartz under the influence of clays has been recognized in sandstones for many years. It is well known that a grain of quartz in contact with a clay flake dissolves faster than when in contact with another grain of quartz. This phenomenon promotes silica transfer during the diagenesis of sandstones and is responsible of deformation and porosity variations. Here we make an attempt to explain the process of this rock deformation using a pressure solution mechanism.

Автор(ы):Борисяк А.А.
Издание:Типо-литография К.Биркенфельда, Санкт-Петербург, 1909 г., 18 стр.
Язык(и)Русский
Pseudomonotis ochotica Tell. Крымско-Кавказского триаса

Исследования Геологического Комитета в Крымском горном кряже доставили немало новых материалов, как для понимания морфологии, так и для тектоники и стратиграфии этих гор. В частности это касается и той песчаноглинистой толщи, которая слагает нижнюю часть склона Южного берега, а также значительныя площади на северном склоне кряжа. Эта толща является то более глинистой, и тогда почти черного цвета, с отдельными известковыми и сферосидеритовыми стяжениями и с пропластами плотных, более или менее железистых песчаников и вулканических туфов, то более песчаной и тогда более светлых цветов, обычно сильно слюдистой и с массой плохо сохраненныхъ растительных остатков; <...>

Редактор(ы):Ehlers J., Gibbard P.
Издание:2004 г., 428 стр.
Язык(и)Русский
Quaternary Glaciations - Extent and Chronology, Part II: North America / Четвертичные оледенения - масштабы и хронология, Часть II: Северная Америка

"Quaternary Glaciations- Extent and Chronology, Part II: North America", edited by Jtirgen Ehlers and Philip Gibbard is the second volume of three, covering Quaternary glaciations across the Earth. Part I covered Europe, and Part III will cover South America, Asia, Africa, Australia and Antarctica. Together these three volumes form the second publication in the Elsevier Book Series on "Developments in Quaternary Science".

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