Shun-ichiro Karato, "Deformation of Earth Materials: An Introduction to the Rheology of Solid Earth"

Shun-ichiro Karato, "Deformation of Earth Materials: An Introduction to the Rheology of Solid Earth"
Cambridge University Press; illustrated edition (March 10, 2008) | English | 0521844045 | 474 pages | PDF | 7.37 MB

Much of the recent progress in the solid earth sciences is based on interpretation of a range of geophysical and geological observations in terms of the properties and deformation of earth materials. This graduate textbook presents a comprehensive, unified treatment of the materials science of deformation as applied to solid earth geophysics and geology. The deformation of Earth materials is presented in a systematic way covering elastic, anelastic and viscous deformation. Advanced discussions on current debates are also included to bring readers to the cutting-edge of science in this interdisciplinary area. This textbook is ideal for graduate courses on the rheology and dynamics of solid Earth, and includes review questions with solutions so readers can monitor their understanding of the material presented. It is also a much-needed reference for geoscientists in many fields including geology, geophysics, geochemistry, materials science, mineralogy and ceramics.

A comprehensive, unified treatment of the materials science of deformation as applied to solid earth geophysics and geology, this textbook is ideal for graduate courses on the rheology and dynamics of solid earth. It is also a much-needed reference for geoscientists in geology, geophysics, geochemistry, materials science, mineralogy and ceramics.

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"Petrology of Sedimentary Rocks, Second Edition" by Sam Boggs, Jr.

"Petrology of Sedimentary Rocks, Second Edition" by Sam Boggs, Jr.
Cambridge University Press | 2009 | ISBN: 0521897165 | 612 pages | PDF | 15 Mb

This Second Edition maintains the fundamental structure of the original book, and presents a comprehensive treatment of sedimentary petrography and petrology. It has been thoroughly updated to include new concepts and ideas, and cutting-edge techniques such as cathodoluminescence imaging of sedimentary rocks and backscattered electron microscopy.

Numerous photographs and diagrams illustrate characteristic features while an extensive and up-to-date reference list provides a useful starting point for additional literature research.

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This textbook is designed for advanced undergraduate and graduate courses in sedimentary petrology. It is also a key reference for researchers and professional petroleum geoscientists wanting to develop an understanding of the petrologic characteristics of sedimentary rocks and their geological significance.

Table of Contents

Part I. Principles:

1. Origin, classification and occurrence of sedimentary rocks;

Part II. Siliciclastic Sedimentary Rocks:

2. Sedimentary textures;

3. Sedimentary structures;

4. Sandstones;

5. Conglomerates;

6. Mudstones and shales;

7. Provenance of siliciclastic sedimentary rocks;

8. Diagenesis of sandstones and shales;

Part III. Carbonate Sedimentary Rocks:

9. Limestones;

10. Dolomites;

11. Diagenesis of carbonate rocks;

Part IV. Other Chemical/Biochemical Sedimentary Rocks and Carbonaceous Sedimentary Rocks:

12. Evaporites, cherts, iron-rich sedimentary rocks, and phosphorites;

13. Carbonaceous sedimentary rocks;

Bibliography;

Index.

Donal M. Ragan, "Structural Geology: An Introduction to Geometrical Techniques"

Donal M. Ragan, "Structural Geology: An Introduction to Geometrical Techniques"
Cambridge University Press | 2009 | ISBN: 0521897580, 0521745837 | 624 pages | PDF | 6,2 MB

This combination of text and lab book presents an entirely different approach to structural geology. Designed for undergraduate laboratory classes, it provides a step-by-step guide for solving geometric problems arising from structural field observations. The book discusses both traditional methods and cutting-edge approaches, with emphasis given to graphical methods and visualization techniques that support students in tackling challenging two- and three-dimensional problems. Numerous exercises encourage practice in using the techniques, and demonstrate how field observations can be converted into useful information about geological structures and the processes responsible for creating them. This updated fourth edition incorporates new material on stress, deformation, strain and flow, and the underlying mathematics of the subject. With stereonet plots and solutions to the exercises available online at www.cambridge.org/ragan, this book is a key resource for undergraduates, advanced students and researchers wanting to improve their practical skills in structural geology.

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Harold Stowell - Geology of Southeast Alaska: Rock and Ice in Motion

Harold Stowell - Geology of Southeast Alaska: Rock and Ice in Motion
Publisher: University of Alaska Press | 2006-03-01 | ISBN: 188996381X | PDF | 152 pages | 5.79 MB

The most powerful forces on earth have shaped the landscape of Southeast Alaska. Scientists and visitors from around the world trek north to experience wild rivers, powerful glaciers, and breathtaking mountain peaks. Now, for the first time, a handy guide to the region is available. Complete with color illustrations revealing millions of years of geological history and in-depth descriptions of Sitka, Juneau, and Glacier Bay, Geology of Southeast Alaska is essential reading for anyone fascinated by rock and ice in motion.

Written by a geologist with over twenty-five years of experience in the north, Geology of Southeast Alaska will entertain and inform with abundant photographs and detailed drawings. Whether you want to understand the forces that shaped the state of Alaska, or you want to learn the basics of glacial movement, this compact, authoritative book is for you.

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"Paleoseismology" ed. by James P. McCalpin

"Paleoseismology" ed. by James P. McCalpin
International Geophysics, Volume 95, Second Edition
Elsevier Inc | 2009 | ISBN: 0123735768 | 802 pages | PDF/djvu | 39/22 Mb

Completely updated version of a book solely devoted to paleoseismology. It summarizes the development of the field from the 1960s to the present. Chapters cover the entire range of techniques currently used in paleoseismic reconstruction.

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Contents

Introduction to Paleoseismology

Field Techniques in Paleoseismology — Terrestrial Environments

Sub-Aqueous Paleoseismology

Paleoseismology in Extensional Tectonic Environments

Paleoseismology of Volcanic Environments

Paleoseismology of Compressional Tectonic Environments

Paleoseismology of Strike-Slip Tectonic Environments

Using Liquefaction-Induced and Other Soft-Sediment Features for Paleoseismic Analysis

Using Landslides for Paleoseismic Analysis

Application of Paleoseismic Data to Seismic Hazard Assessment and Neotectonic Research

Andrew D. Miall The Geology of Stratigraphic Sequences, Second Edition

Andrew D. Miall The Geology of Stratigraphic Sequences, Second Edition
Springer | 2010 | ISBN : 3642050263 | 864 pages | PDF | 27,7 MB

It has been more than a decade since the appearance of the First Edition of this book. Much progress has been made, but some controversies remain. The original ideas of Sloss and of Vail (building on the early work of Blackwelder, Grabau, Ulrich, Levorsen and others) that the stratigraphic record could be subdivided into sequences, and that these sequences store essential information about basin-forming and subsidence processes, remains as powerful an idea as when it was first formulated. The definition and mapping of sequences has become a standard part of the basin analysis process. The main purpose of this book remains the same as it was for the first edition, that is, to situate sequences within the broader context of geological processes, and to answer the question: why do sequences form? Geoscientists might thereby be better equipped to extract the maximum information from the record of sequences in a given basin or region. Tectonic, climatic and other mechanisms are the generating mechanisms for sequences ranging over a wide range of times scales, from hundreds of millions of years to the high-frequency sequences formed by cyclic processes lasting a few tens of thousands of years

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John P. Rafferty, "The Paleozoic Era: Diversification of Plant and Animal Life"

John P. Rafferty, "The Paleozoic Era: Diversification of Plant and Animal Life"
Rosen Education Service | 2010 | ISBN: 1615301119, 1615301968 | 339 pages | PDF | 6,3 MB

Introduction:

The Paleozoic Era is probably less familiar and perhaps

less dramatic than the age of the dinosaurs that would

dominate the Mesozoic Era that followed. However, the

Paleozoic Era contained one of the most intense increases

in biodiversity in Earth’s history, the Cambrian explosion

and the subsequent Ordovician radiation. It also contained

the largest extinction event the world has ever

known, the Permian extinction, which wiped out more

than 90 percent of marine species and roughly 70 percent

of species on land. It was also a time of great geological

changes as landmasses migrated and collided, eventually

creating the supercontinent called Pangea. Sea levels rose,

drowning whole continents, fell, and rose again. Some of

Earth’s oldest mountain ranges, such as the Appalachians

and the Urals, were formed during the Paleozoic. Life

moved from the oceans to dry land and insects took wing

for the first time. Many evolutionary advances took place,

which set the stage for life as we know it today. Some of

these advances include the development of plants with

seeds, shelled eggs, and organisms capable of breathing

air. So in geologic history the Paleozoic Era was pretty

dramatic after all. In the pages that follow, all of these

developments, as well as the clues that scientists have used

to decipher the history of Earth’s changes, will be explored.

Spanning nearly 300 million years of history, from 542

to 251 million years ago, the Paleozoic Era covers more

than half of the Phanerozoic Eon, also known as the Age

of Life—the geologic time in which humans still live.

Scientists divide the Paleozoic into a number of smaller

periods, beginning with the Cambrian, approximately 542

million to 488 million years ago, followed by the

Ordovician, Silurian, Devonian, Carboniferous, and

Permian periods. Most of these names are derived from

the locations in which rocks and fossils from that time

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Soils in Archaeological Research By Vance T. Holliday

Soils in Archaeological Research By Vance T. Holliday
Publisher: OUP 2004 | 464 Pages | ISBN: 0195149653 | PDF | 6 MB

Soils, invaluable indicators of the nature and history of the physical and human landscape, have strongly influenced the cultural record left to archaeologists. Not only are they primary reservoirs for artifacts, they often encase entire sites. And soil-forming processes in themselves are an important component of site formation, influencing which artifacts, features, and environmental indicators (floral, faunal, and geological) will be destroyed and to what extent and which will be preserved and how well. In this book, Holliday will address each of these issues in terms of fundamentals as well as in field case histories from all over the world. The focus will be on principles of soil geomorphology , soil stratigraphy, and soil chemistry and their applications in archaeological research.

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W. Schwarzacher, "Cyclostratigraphy and the Milankovitch Theory (Developments in Sedimentology)"

W. Schwarzacher, "Cyclostratigraphy and the Milankovitch Theory (Developments in Sedimentology)"
Publisher: Elsevier Science | 1993 | ISBN 0444896236 | PDF | 238 pages | 11.5 MB

Hardbound. Cyclostratigraphy is concerned primarily with measuring geological time and the time units used in this approach are sedimentary cycles. Milankovitch cycles mark time intervals of tens of thousands to several millions of years. Such cycles are the result of variations in the Earth's position in relation to the Sun and these in turn determine the climatic variations. The Milankovitch theory was resurrected in the 1960's when evidence from Pleistocene deep sea sediments linked orbital variations and climate.

This monograph discusses sedimentary cycles and their use in measuring geologic time. There is considerable effort made to clarify the term "sedimentary cycle", in particular, the two opposing concepts of cyclic stratification and event stratification. The recognition of sedimentary cycles and of Milankovitch cycles specifically, is considered and care is taken with the question of relating sediment thickness to time.

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