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Издание 7
Автор(ы):Greensmith J.T.
Издание:Unwin Hyman, 1989 г., 270 стр., ISBN: 978-94-011-9642-0
Язык(и)Английский
Petrology of the sedimentary rocks / Петрология осадочных горных пород

Sediments are formed of materials deposited episodically from water, air and ice, as well as soils, coals and volcanic detritus. Compaction, cementation and burial processes lithify loose sediments into sedimentary rocks and occasionally mask the character of the original deposit. Fortunately, many lithified rocks possess qualities so similar to those of modern deposits.that the conditions under which they formed can be determined with some certainty. When fossil remains and traces exist, such determinations are greatly facilitated. On the other hand, there are sedimentary rocks, such as banded iron-formations and chalks, which can be described accurately but which still defy completely satisfactory genetic interpretation, because there are no clear modern equivalents. <...>

Издание 2
Автор(ы):Boggs S.
Издание:Cambridge University Press, 2009 г., 611 стр., ISBN: 978-0-511-71933-2
Язык(и)Английский
Petrology of the sedimentary rocks / Петрология осадочных горных пород

Sedimentary rocks form at low temperatures and pressures at the surface of Earth owing to deposition by water, wind, or ice. By contrast, igneous and metamorphic rocks form mainly below Earth’s surface where temperatures and pressures may be orders of magnitude higher than those at the surface, although volcanic rocks eventually cool at the surface. These fundamental differences in the origin of rocks lead to differences in physical and chemical characteristics that distinguish one kind of rock from another. Sedimentary rocks are characterized particularly by the presence of layers, although layers are also present in some volcanic and metamorphic rocks, and by distinctive textures and structures. Many sedimentary rocks are also distinguished from igneous and metamorphic rocks by their mineral and chemical compositions and fossil content.

Издание 2
Автор(ы):Blatt H., Tracy R.J.
Издание:W.H. Freeman and Company Publishers, New York, 1996 г., 544 стр., ISBN: 0-7167-2438-3
Язык(и)Английский
Petrology. Igneous, sedimentary and metamorphic / Петрология. Изверженные, осадочные и метаморфические породы

Leaving aside the atmosphere and hydrosphere, rocks are the stuff of which the earth is made. Because of this, the study of rocks, petrology (from the Greek petra, “rock,” and logos, “discourse or explanation”), occupies a central position among the earth sciences. The study of rocks is the source of virtually all of our ideas about the history of Earth. Knowledge about rocks, their origin and ages, and their distribution is potentially capable of contributing to the solution of a wide variety of problems that run the gamut of geological interests.

Автор(ы):Sen G.
Издание:Springer, 2014 г., 369 стр., ISBN: 978-3-642-38799-9
Язык(и)Английский
Petrology. Principles and practice / Петрология. Принципы и практика

It is always easier to write a textbook the second time around, or so I thought. Writing my first textbook entitled “Earth’s Materials: Minerals and Rocks” (published in 2001 by Prentice-Hall) was difficult because I had to make some tough decisions about what materials to include and what to leave out. Based on my own thinking and input from colleagues and students since that time, I decided to write a textbook on petrology and leave out mineralogy altogether. The result is the present textbook. It was anything but easy to write this book.

ТематикаПетрология
Издание:American Association of Petroleum Geologists, 2006 г., 212 стр., ISBN: 978-0-89181-750-5
Язык(и)Английский
Petrophysical evaluation of hydrocarbon pore-thickness in thinly bedded clastic reservoirs / Петрофизическая оценка толщины углеводородных пор в тонкослойных терригенных коллекторах

This chapter describes the difficulties associated with formation evaluation in thinly bedded sandstone reservoirs and outlines the existing technology that has been applied to these difficulties. Chapter 2 introduces our integrated approach to evaluating hydrocarbon pore-thickness in thinly bedded clastic reservoirs.

Many terms are introduced in these two chapters through examples and informal definitions: for example, earth models, bed types, logging tool forward models, convolution, inversion, statistical earth models, and Monte Carlo inversion. These topics are discussed more thoroughly in Chapters 6 through 10, and the integrated approach is described in detail in Chapters 11 through 13. <...>

Автор(ы):Peters E.J.
Издание:Austin, 2007 г., 1048 стр.
Язык(и)Английский
Petrophysics / Петрофизика

Petrophysics is the study of rock properties and their interactions with fluids (gases, liquid hydrocarbons and aqueous solutions). Because petroleum reservoir rocks must have porosity and permeability, we are most interested in the properties of porous and permeable rocks. The purpose of this text is to provide a basic understanding of the physical properties of permeable geologic rocks and the interactions of the various fluids with their interstitial surfaces. Particular emphasis is placed on the transport properties of the rocks for single phase and multiphase flow. <...>

Издание 4
Автор(ы):Donaldson E.C., Tiab D.
Издание:Elsevier, 2016 г., 919 стр., ISBN: 978-0-12-803188-9
Язык(и)Английский
Petrophysics theory and practice of measuring reservoir rock and fluid transport properties / Петрофизика, теория и практика измерения свойств пород-коллекторов и транспорта флюидов

Petrophysics is the study of rock properties and their interactions with fluids (gases, liquid hydrocarbons, and aqueous solutions). The geologic material forming a reservoir for the accumulation of hydrocarbons in the subsurface must contain a three-dimensional network of interconnected pores in order to store the fluids and allow for their movement within the reservoir.

Автор(ы):Cannon S.
Издание:Wiley Blackwell, 2016 г., 216 стр., ISBN: 978-1-118-74674-5
Язык(и)Английский
Petrophysics: A practical guide / Петрофизика: Практическое руководство

This book has been written for those studying petroleum geology or engineering, for whom the role of the petrophysicist can become a lucrative and satisfying career. The handbook will be equally useful to students and practioners of environmental science and hydrogeology, where the understanding of groundwater flow is an important part of their technical remit.

Издание:2018 г., 19 стр.
Язык(и)Английский
PGE–(REE–Ti)-Rich Micrometer-Sized Inclusions, Mineral Associations, Compositional Variations, and a Potential Lode Source of Platinum-Group Minerals in the Sisim Placer Zone, Eastern Sayans, Russia

Обогащенные PGE–(REE–Ti) элементами включения микрометрового размера, минеральные ассоциации, вариации состава и потенциальный источник минералов платиновой группы в россыпной зоне Сисим, Восточные Саяны, Россия.

We report the results of a mineralogical investigation of placer samples from the upper reaches of the Sisim watershed, near Krasnoyarsk, in Eastern Sayans, Russia. The placer grains are predominantly Os–Ir–(Ru) alloys (80%) that host various inclusions (i.e., platinum-group elements (PGE)-rich monosulfide, PGE-rich pentlandite, Ni–Fe–(As)-rich laurite, etc.) and subordinate amounts of Pt–Fe alloys.

Автор(ы):Gasparik T.
Издание:Springer, 2014 г., 466 стр., ISBN: 978-1-4614-5775-6
Язык(и)Английский
Phase diagrams for geoscientists / Фазовые диаграммы в науках о земле

This book summarizes the results of the experimental studies of phase relations in the chemical systems relevant to Earth, carried out by the author in a time period of over 20 years between 1979 and 2001. It is based on 1,000 pistoncylinder experiments at pressures up to 4 GPa and close to 700 experiments carried out with a multi-anvil apparatus at pressures up to 24 GPa. The emphasis in these studies was on internal consistency. Large sets of data were produced using the same sample assembly, high-pressure apparatus, experimental procedures and calibrations by the same experimentalist to maximize the internal consistency. The results were published in 70 peer-reviewed articles listed at the end of the book. These are referenced only by the corresponding number, while the full reference is given for all other sources. <...>

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