Metamorphic rocks are one of the three main types of rock. Originally comprising either igneous or sedimentary rocks, metamorphic rocks are the products of change by heat and pressure, often at great depths in the earth's crust, into a completely new form. One of the classic examples of the result of a metamorphic process is the transformation of sedimentary mudstone into slate.Introducing Metamorphism provides a succinct introduction to metamorphism. Ian Sanders explains how and why rocks change during metamorphic processes. He discusses the role of water in metamorphism and describes the different types of metamorphic processes including contact, shock and high pressure metamorphism and metamorphism in an orogenic belt.Copiously illustrated and written for those who wish to gain a clear understanding of metamorphic processes, Introducing Metamorphism is designed to make the processes that led to the formation of these rocks intelligible to its readers. Technical terms are kept to a minimum and are explained in a glossary.

This rigorous and up-to-date synthesis of current research and thought in igneous petrology explores the complex process of the generation and cooling of igneous rocks--those formed by solidification from a molten state, either intrusively, below the earth's crust, or extrusively as lava. Through the study of the mineral associations, compositions, and textures achieved in the formation of these rocks, Paul Hess traces the evolution of igneous rocks from site of origin to place of residency. He probes the clues that the distribution of igneous rocks provides for understanding plate tectonic processes. And he focuses on a number of unresolved problems critical to igneous petrology: the ultimate source rock of a magma; the location and process of melting; the collection of magma into large movable masses; the extraction of magma from its source and its emplacement onto the earth's crust; and the conditions of the crystallization and cooling of magma in its ultimate transformation into igneous rock. This comprehensive work, which integrates geochemistry, tectonophysics, and planetary geology with classical igneous petrology, provides a solid introduction to physical processes and isotopic principles and applies these processes and principles consistently in the discussion of petrogenetic models for all the major types of igneous rocks. It is a stimulating resource for students and researchers in igneous petrology as well as for geologists in allied fields (geophysics, geochemistry, cosomochemistry, and metamorphic petrology).

All Earth Science students need to understand the origins, environments, and basic processes that produce igneous and metamorphic rocks. This concise introductory textbook provides students with the essential knowledge needed to understand how petrology relates to other topics in the geologic sciences, and has been written specifically for one-semester courses. Throughout, the emphasis is on interpreting the mineralogy and petrology of rock suites in terms of origin and environment, with the first half of the book concentrating on igneous rocks, and the second half on metamorphic rocks. This Second Edition has been thoroughly revised and brought completely up-to-date. It now includes a new chapter on the application of stable and radiogenic isotopes in petrology, introducing students to the concept of isotopic fractionation and describing the process of radioactive decay. The discussions of phase diagrams, connections between igneous and metamorphic rock suites, and convergent margin magmatism have also been expanded. There is a new glossary of terms, updated end-of-chapter exercises, and updated further readings.

Petrogenesis of Metamorphic Rocks presents a large number of diagrams showing the stability relations among minerals and groups of minerals found in metamorphic rocks. The diagrams help to determine the pressure and temperature conditions under which a given set of metamorphic rocks may have formed. Other parameters that control metamorphic mineral assemblages are also discussed and pitfalls resulting from simplifications and generalizations are highlighted. The book discusses the most common metamorphic rock types, their nomenclature, structure and graphical representation of their mineral assemblages.

Part I defines basic principles of metamorphism, introduces metamorphic processes, geologic thermometry and barometry and defines metamorphic grade. Part II presents in a systematic way mineralogical changes and assemblages found in the most common types of metamorphic rocks. The computation of diagrams is based on recent advances in quantitative petrology and geochemistry. An extensive bibliography, including the key contributions and classic papers in the field, make it an invaluable source book for graduate students and professional geologists.

The papers compiled in this book cover almost all aspects of in-situ characterization ranging from rock mass classification measurement of in-situ stresses, strength and deformation characteristics to field instrumentation and back analysis of observations made.

Regolith is the layer of broken and unconsolidated rock and soil material that forms the surface of the land and covers the bedrock nearly everywhere. An understanding of its properties and structure is very important in topics such as groundwater supply, soil conservation and exploration efforts for economic materials. Regolith, Soils and Landforms is a manual for students, professionals and researchers concerned with the practical examination and analysis of earth surface materials in the field. The text describes many economic aspects of regolith studies, such as the formation of mineral deposits, the importance of weathering zones and how the chemistry of regolith affects human health. Presenting a new view of the geological history of the earth, it places emphasis on the formation and destruction of regolith materials and provides a challenge for established concepts in landscape evolution. It will be an essential text to a wide range of readership including students of Geology, Geomorphology, Geography, Agriculture and Engineering as well as professionals dealing with regolith in their own work.

Many common terms in metamorphic petrology vary in their usage and meaning between countries. The International Union of Geological Sciences (IUGS) Subcommission on the Systematics of Metamorphic Rocks (SCMR) has aimed to resolve this, and to present systematic terminology and rock definitions that can be used worldwide. This 2007 book is the result of discussion and consultation lasting 20 years and involving hundreds of geoscientists worldwide. It presents a complete nomenclature of metamorphic rocks, with a comprehensive glossary of definitions, sources and etymology of over 1200 terms, and a list of mineral abbreviations. Twelve multi-authored sections explain how to derive the correct names for metamorphic rocks and processes, and discuss the rationale behind the more important terms. These sections deal with rocks from high- to low- and very-low-grade. This book will form a key reference and international standard for all geoscientists studying metamorphic rocks.

This encyclopedia, which constitutes a wide ranging and authoritative collection of academic articles, covers the sedimentological aspects of sediments and sedimentary rocks. As such the encyclopedia provides a comprehensive, one-volume reference work for students and faculty in universities, and for professionals in geology and allied disciplines (geography, engineering, environmental studies), as well as informed lay readers.

This book presents the proceedings of the 30th International Geological Congress, covering oil and gas generation in nonmarine basins, targets of hydrocarbons, reservoir characterization, marine carbonate source beds, and oil and gas basin system.

Oil exploration requires proper understanding of the geological set-up of any area to make the process economical and effective. This involves geological, geophysical, geochemical surveys including studying the lateral variations in litho-stratigraphic units in the adjoining areas surrounding the bore-hole, done through study of Dipmeter logs. This book 'Dipmeter Surveys in Petroleum Exploration' giving all the required backup of the other allied subjects for easy and meaningful interpretations of the Dipmeter data, so that drilling of dry wells is avoided to maximum possible extent and new discoveries to be made, thereby enhancing the oil resource of a particular geographical location.

These three works cover the entire field of formation evaluation, from basic concepts and theories, through standard methods used by the petroleum industry, on to new and exciting applications in environmental science and engineering, hydrogeology, and other fields. Designed to be used individually or as a set, these volumes represent the first comprehensive assessment of all exploration methodologies. No other books offer the breadth of information and range of applications available in this set.

This is a translation of "Fazovie Prevrazheniya i Petrogenez." Earthquakes, tectonic movements and magmatic activities are considered as different manifestations of the same physico-mechanical process. This text discusses characteristics of phase transformation thermodynamics and the origin of magmaic fomrations are discussed.

This is the first book ever published on the problems of true triaxial testing of rocks addressing all aspects of true triaxial testing of rocks, including: (i) true triaxial testing techniques and procedures; (ii) test results: strength, deformability, failure mode, permeability, acoustic emission, and elastic wave velocity; (iii) constitutive laws and failure criteria; and (iv) applications to geoengineering and geosciences.

Recent developments in the field of true triaxial testing of rocks are presented, as well as a thorough review of the most important achievements in the whole history of true triaxial testing of rocks.

Almost all researchers from around the world engaged in the true triaxial testing of rocks over the last three decades have contributed to this work. The authors originate from different branches of geoengineering and geosciences, including civil engineering, engineering geology, geotechnical engineering, mining engineering, petroleum engineering, seismology, and tectonophysics.

Fission track dating is based on the microscopic observation and counting of etchable tracks left by the spontaneous fission of uranium in minerals. Since its development in 1963 the method attracted a steadily growing interest from geologists and geochronologists throughout the world. Apart from its relative experimental ease the success must be mainly ascribed to the specific ability of the method of unravelling the thermal and tectonic history of rocks, a potential which only became fully exploited during the last decade with the systematic introduction of track size analysis. This work deals with fission track dating covering all of its aspects from the origin of the fission tracks, the basis of track etching and fading, the various dating techniques as well as practical procedures and the geologic interpretation to recent applications in geology and archaeology.

Progress in Rock Physics: New Developments in Theory and Experiment on Wave Propagation in Porous Rocks provides a thorough and highly valuable review on the latest contributions of rock physics research. The features, applicability and shortcomings of theoretical models are discussed in detail, aiding the reader in their research and engineering work. This book outlines six central topics of wave propagation theory in porous rocks: visco-elasticity, anisotropy, squirt flow, patchy saturation, double-porosity and nonlinear acoustics. The latest results of effective medium theory and experimental measurements are also discussed.