Dissertation Abstracts International
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Published: 2005
Total Pages: 794
ISBN-13:
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Exhumation Processes
Author: Uwe Ring
Publisher: Geological Society of London
Published: 1999
Total Pages: 390
ISBN-13: 9781862390324
DOWNLOAD EBOOKOdysseus Unbound
Author: Robert Bittlestone
Publisher: Cambridge University Press
Published: 2005-09-19
Total Pages: 636
ISBN-13: 9780521853576
DOWNLOAD EBOOKExtraordinary story of the exciting discovery of the true location of Odysseus' homeland of Ithaca.
Quaternary Sea-Level Changes
Author: Colin V. Murray-Wallace
Publisher: Cambridge University Press
Published: 2014-01-30
Total Pages: 503
ISBN-13: 0521820839
DOWNLOAD EBOOKAn important overview of Quaternary climates including detailed Pleistocene and Holocene sea-level changes, for researchers and graduate and advanced undergraduate students.
Metasomatism and the Chemical Transformation of Rock
Author: Daniel Harlov
Publisher: Springer Science & Business Media
Published: 2012-08-14
Total Pages: 804
ISBN-13: 3642283934
DOWNLOAD EBOOKFluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth’s continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Metasomatic processes can include ore mineralization, metasomatically induced alteration of oceanic lithosphere, mass transport in and alteration of subducted oceanic crust and overlying mantle wedge, which has subsequent implications regarding mass transport, fluid flow, and volatile storage in the lithospheric mantle overall, as well as both regional and localized crustal metamorphism. Metasomatic alteration of accessory minerals such as zircon or monazite can allow for the dating of metasomatic events as well as give additional information regarding the chemistry of the fluids responsible. Lastly present day movement of fluids in both the lithospheric mantle and deep to mid crust can be observed utilizing geophysical resources such as electrical resistivity and seismic data. Such observations help to further clarify the picture of actual metasomatic processes as inferred from basic petrographic, mineralogical, and geochemical data. The goal of this volume is to bring together a diverse group of geologists, each of whose specialities and long range experience regarding one or more aspects of metasomatism during geologic processes, should allow them to contribute to a series of review chapters, which outline the basis of our current understanding of how metasomatism influences and helps to control both the evolution and stability of the crust and lithospheric mantle.
Geochronology
Author: Derek Vance
Publisher: Geological Society of London
Published: 2003
Total Pages: 278
ISBN-13: 9781862391468
DOWNLOAD EBOOKIsotope geochemistry has produced many technical developments recently that have revolutionised the potential information available on the tectonics of metamorphic belts from geochronology. This set of papers describes recent progress in integrating this new information with other datasets from metamorphic petrology on a mineral and sub-mineral scale.
Volcanic Successions Modern and Ancient
Author: R. Cas
Publisher: Springer Science & Business Media
Published: 2012-12-06
Total Pages: 532
ISBN-13: 9400931670
DOWNLOAD EBOOKOne of our aims in the book is to provide geologists with a sound basis for making their own well founded interpretations. For that reason we cover not only concepts about processes, and the nature of the products, but also methods and approaches that may be useful in analysing both modern and ancient successions. Most importantly, we treat the diversity of products in volcanic terrains as facies, and we use the method of facies analysis and interpretation as a means of constructing facies models for different volcanic settings. These models will, we hope, be useful as norms for comparison for workers in ancient terrains. The idea for this book came into being between 1981 and 1982 when J. V. W. came to Monash University to take up a Monash Postdoctoral Fellowship. During this period a short course on facies analysis in modern and ancient successions was put together, integrating J.V.W.'s extensive volcanological experience in numerous modern volcanic terrains with R.A.F.C.'s extensive sedimentological and volcanological experience in older volcanic and associated sedimentary successions in the Palaeozoic and Precambrian of Australia. The enthusiastic response from the participants to the first short course, taught in May 1982, and to subsequent annual re-runs, encouraged us to develop the short course notes into this book. The idea for both the short course and the book arose because we felt that there was no single source available that comprehensively attempted to address the problems of analysing, interpreting and understanding the complexity of processes, products and stratigraphy in volcanic terrains.
Petrogenesis of Metamorphic Rocks
Author: Kurt Bucher
Publisher: Springer Science & Business Media
Published: 2013-04-17
Total Pages: 298
ISBN-13: 3662030004
DOWNLOAD EBOOKMetamorphic rocks are one of the three classes of rocks. Seen on a global scale they constitute the dominant material of the Earth. The understanding of the petrogenesis and significance of metamorphic of geological education. rocks is, therefore, a fundamental topic There are, of course, many different possible ways to lecture on this theme. This book addresses rock metamorphism from a relatively pragmatic view point. It has been written for the senior undergrad uate or graduate student who needs practical knowledge of how to interpret various groups of minerals found in metamorphic rocks. The book is also of interest for the non-specialist and non-petrolo gist professional who is interested in learning more about the geolo gical messages that metamorphic mineral assemblages are sending, as well as pressure and temperature conditions of formation. The book is organized into two parts. The first part introduces the different types of metamorphism, defines some names, terms and graphs used to describe metamorphic rocks, and discusses principal aspects of metamorphic processes. Part I introduces the causes of metamorphism on various scales in time and space, and some principles of chemical reactions in rocks that accompany metamorphism, but without treating these principles in detail, and presenting the thermodynamic basis for quantitative analysis of reactions and their equilibria in metamorphism. Part I also presents concepts of metamorphic grade or intensity of metamorphism, such as the metamorphic-facies concept.
The Role of Halogens in Terrestrial and Extraterrestrial Geochemical Processes
Author: Daniel E. Harlov
Publisher: Springer
Published: 2018-01-30
Total Pages: 1029
ISBN-13: 3319616676
DOWNLOAD EBOOKThe book summarizes the knowledge and experiences concerning the role of halogens during various geochemical processes, such as diagenesis, ore-formation, magma evolution, metasomatism, mineralization, and metamorphism in the crust and mantle of the Earth. It comprises the role of halogens in other terrestrial worlds like volatile-rich asteroids, Mars, and the ice moons of Jupiter and Saturn. Review chapters outline and expand upon the basis of our current understanding regarding how halogens contribute to the geochemical/geophysical evolution and stability of terrestrial worlds overall.
Hypogene Karst Regions and Caves of the World
Author: Alexander Klimchouk
Publisher: Springer
Published: 2017-08-17
Total Pages: 903
ISBN-13: 3319533487
DOWNLOAD EBOOKThis book illustrates the diversity of hypogene speleogenetic processes and void-conduit patterns depending on variations of the geological environments by presenting regional and cave-specific case studies. The cases include both well-known and newly recognized hypogene karst regions and caves of the world. They all focus on geological, hydrogeological, geodynamical and evolutionary contexts of hypogene speleogenesis. The last decade has witnessed the boost in recognition of the possibility, global occurrence, and practical importance of hypogene karstification (speleogenesis), i.e. the development of solutional porosity and permeability by upwelling flow, independent of recharge from the overlying or immediately adjacent surface. Hypogene karst has been identified and documented in many regions where it was previously overlooked or misinterpreted. The book enriches the basis for generalization and categorization of hypogene karst and thus improves our ability to adequately model hypogene karstification and predict related porosity and permeability. It is a book which benefits every researcher, student, and practitioner dealing with karst.
