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Автор(ы):Allen J.R.L.
Издание:Elsevier, 1982 г., 612 стр., ISBN: 0-444-41935-7
Язык(и)Английский
Sedimentary structures. Their character and physical basis. Volume 1 / Осадочные структуры. Их характеристики и физические основы. Том 1

Sedimentary structures arise in immediate or close association with the transport of sedimentary materials. Some form where erosion predominates, others as net deposition prevails, and yet further kinds in the brief interval of time between sediment deposition and significant lithification. Many sedimentary structures are ordered features visible on sedimentation (bedding) surfaces, whereas others, often related to surface forms, are expressed as compositional and/or textural patterns (stratification) within Sedimentary deposits. Sedimentary structures can be created by chemical and biological as well as by physical agencies, but this book is about those structures wholly or predominantly shaped by physical mechanisms. The latter are much the most important and have continued to attract attention since the earliest days of the earth sciences in their modern form. <...>

Автор(ы):Allen J.R.L.
Издание:Elsevier, 1982 г., 678 стр., ISBN: 0-444-41935-7
Язык(и)Английский
Sedimentary structures. Their character and physical basis. Volume 2 / Осадочные структуры. Их характеристики и физические основы. Том 2

As the General Preface accompanying Volume I contains an introduction to the work as a whole, it is only necessary for me here to outline the scope of the second volume.
Volume I1 is about sedimentary structures found in relatively complex physical settings, where groupings or hierarchies of features are often of most interest, and more emphasis is placed than in the first volume on cohesive as opposed to cohesionless beds. Secondary currents can exist for a number of reasons in boundary-layer flows, giving rise to flow-parallel sedimentary structures on both kinds of bed.

Издание 2
Автор(ы):Nichols G.
Издание:Wiley Blackwell, 2009 г., 431 стр., ISBN: 978-1-4051-3592-4
Язык(и)Английский
Sedimentology and stratigraphy / Седиментология и стратиграфия

Sedimentology is the study of the processes of formation, transport and deposition of material that accumulates as sediment in continental and marine environments and eventually forms sedimentary rocks. Stratigraphy is the study of rocks to determine the order and timing of events in Earth history: it provides the time frame that allows us to interpret sedimentary rocks in terms of dynamic evolving environments. The stratigraphic record of sedimentary rocks is the fundamental database for understanding the evolution of life, plate tectonics through time and global climate change.

Издание 2
Автор(ы):Alsharhan A.S., Nairn A.E.M.
Издание:Elsevier, 2003 г., 978 стр., ISBN: 0-444-82465-0
Язык(и)Английский
Sedimetary basin and petroleum geology of the middle east / Осадочный бассейн и нефтяная геология Ближнего Востока

The countries of the Middle East (Fig. 1.1), the region reviewed in this book, cover parts of the lands of the eastern Mediterranean and the greater part of Arabia (Arabian Shield, Arabian Platform and Arabian Gulf), and the western Zagros Thrust Zone, an area enclosed between 13 ° and 38 ° N and 35 ° and 60 ° E (Figs. 1.2 and 1.3). Topographically, the higher elevations generally lie to the west in the Arabian Shield and pass eastward into the lower-lying areas occupied by the Arabian (Persian) Gulf and the Tigris-Euphrates Valley.

Автор(ы):Bacon M, Simm R.
Издание:Cambridge University Press, 2014 г., 282 стр., ISBN: 978-1-107-01150-2
Язык(и)Английский
Seismic amplitude. An Interpreters handbook / Сейсмические амплитуды. Руководство по интерпретации

The oil and gas industries now routinely use seismic amplitudes in exploration and production as they yield key information on lithology and fluid fill, enabling interpretation of reservoir quality and likelihood of hydrocarbon presence. The modern seismic interpreter must be able to deploy a whole range of sophisticated geophysical techniques, such as seismic inversion, AVO (amplitude variation with offset), and rock physics modelling, as well as integrating information from other geophysical techniques and well data.

Редактор(ы):Goudswaard W., Jenyon M.K.
Издание:European association of exploretion geophysicsts, 1988 г., 292 стр.
Язык(и)Английский
Seismic atlas of structural and stratigraphic features / Сейсмический атлас структурных и стратиграфических особенностей

This Atlas is designed to be a useful work of reference in an easily-handled format amenable to future expansion both by the E.A.E.G. and the users themselves. It is intended for geoscientists in both the industrial and academic spheres who are at an early career stage, and who would find it of value to see how the interpretation of a wide variety of types of structure is approached on actual examples. The notes accompanying the examples have been kept as concise as is consistent with clarity, and some guidance for further study has been given in the form of a list of key words, and brief references with each group of examples; these in turn will open up the literature.

Автор(ы):Chopra S., Marfurt K.J.
Издание:Society of exploration geophysicists, 2006 г., 233 стр., ISBN: 1-56080-086-0
Язык(и)Английский
Seismic attribute mapping of structure and stratigraphy  / Сейсмическое атрибутивное картирование структур и стратиграфицированных образований

This book, Seismic Attribute Mapping of Structure and Stratigraphy, by Satinder Chopra and Kurt J. Marfurt, is designed specihcally as a companion to Marfurt’s 2006 DISC presentation of the same title and is composed primarily of figures from a forthcoming SEG book by the same authors, Seismic Attributes for Prospect Identification and Reservoir Characterization.

Автор(ы):Chopra S., Marfurt K.J.
Издание:Society of exploration geophysicists, 2007 г., 478 стр., ISBN: 0-931830-41-9
Язык(и)Английский
Seismic attributes for prospect identification and reservoir characterization / Сейсмические характеристики для определения перспектив и характеристики коллектора

This work began while Satinder Chopra worked for Coherence Technology Company (CTC), which later became part of Core Laboratories. Chopra is particularly indebted to Vasudhaven Sudhakar (Sudha), who first introduced him to coherence-cube technology. Sudhakar’s belief in Chopra’s abilities sustained him in this work, wherein the intriguing and fascinating aspects of an emerging technology are revealed. Chopra also is indebted to his former CTC/Core Laboratories colleagues Bob Stevens, Laura Evins, and Vladimir Alexeev, who were always willing to help. Thane McKay and Rob Howey have been particularly encouraging and supportive of this writing effort and are gratefully acknowledged. Several examples included in the text have been borrowed from the work of Chopra’s other former colleagues, which he and Kurt J. Marfurt gratefully acknowledge. <...>

Автор(ы):Onajite E.
Издание:Elsevier, 2014 г., 231 стр., ISBN: 978-0-12-420023-4
Язык(и)Английский
Seismic data analysis techniques in hydrocarbon exploration / Методы анализа сейсмических данных при разведке углеводородов

Seismic data have become an important tool for development of oil and gas field as well as for monitoring oil and/or gas production and not just as an exploration tool. Because of the importance of seismic data to the oil and gas industry, graduate geoscientists need to have a clear understanding of seismic data.

Том 2, Издание 2
Автор(ы):Yilmaz O.
Редактор(ы):Doberty S.M.
Издание:Society of exploration geophysicists, 2001 г., 1054 стр., ISBN: 0-931830-46-X
Язык(и)Английский
Seismic data analysis. Processing, inversion and interpretation of seismic data. Volume 2 / Анализ сейсмических данных. Обработка, инверсия и интерпретация сейсмических данных. Том 2

Subsurface geological features of interest in hydrocarbon exploration are three dimensional in nature. Examples include salt diapirs, overthrust and folded belts, major unconformities, reefs, and deltaic sands. A two-dimensional (2-D) seismic section is a cross-section of a three-dimensional (3-D) seismic response. Despite the fact that a 2-D section contains signal from all directions, including out-of-plane of the profile, 2-D migration normally assumes that all the signal comes from the plane of the profile itself.

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