This unparelleled reference synthesizes the methods used in microfacies analysis and details the potential of microfacies in evaluating depositional environments and diagenetic history, and, in particular, the application of microfacies data in the study of carbonate hydrocarbon reservoirs and the provenance of archaeological materials. Nearly 230 instructive plates (30 in color) showing thin-section photographs with detailed explanations form a central part of the content. Helpful teaching-learning aids include detailed captions for hundreds of microphotographs, boxed summaries of technical terms, many case studies, guidelines for the determination and evaluation of microfacies criteria, self-testing exercises for recognition and characterization skills, and more

This book provides a showcase for the incredibly well-preserved flight-textured tektites of southern Australia, which are the world's finest known examples. It provides an overview of their forms and flight features, which can be expected to appear, at least in part, on any objects falling from space. Some of these specimens are so perfectly shaped that it is hard to believe that they have been buried in the recent strata of Australia for 770,000 years. It also discusses the history of the story of their incredible flight into space and return becoming widely accepted, which led to them being recognized as space travelers. Further, it describes their classical shapes and offers an explanation of how each developed. It provides collectors, meteoriticists, and museum curators with insights into the astounding forms of Australian tektites produced by hypersonic flight.

Naturliche Stoffkreislaufe weisen teilweise sehr komplizierte Ruckkopplungsmechanismen auf. Geochemie und "Umwelt" beschreibt solche Regelkreislaufe in der Atmosphare, der Pedosphare, der Anthroposphare und der Hydrosphare. Ein klares Konzept und die Konzentration auf wichtige und aktuelle Forschungsschwerpunkte kennzeichnen die Beitrage, die von fuhrenden Wissenschaftlern der Umweltgeochemie verfasst sind. Das Buch ist nicht nur Ausbildungsstandard fur Studenten und Hochschullehrer, sondern liefert auch Praktikern das aktuelle Wissen fur ihre Arbeit."

This handbook is a reference guide for selecting and carrying out numerous methods of soil analysis. It is written in accordance with analytical standards and quality control approaches. It covers a large body of technical information including protocols, tables, formulae, spectrum models, chromatograms and additional analytical diagrams. The approaches are diverse, from the simplest tests to the most sophisticated determination methods.

This edited work contains the most recent advances related to the study of layered intrusions and cumulate rocks formation. The first part of this book presents reviews and new views of processes producing the textural, mineralogical and geochemical characteristics of layered igneous rocks. The second part summarizes progress in the study of selected layered intrusions and their ore deposits from different parts of the world including Canada, Southwest China, Greenland and South Africa. Thirty experts have contributed to this update on recent research on Layered Intrusions. This highly informative book will provide insight for researchers with an interest in geology, igneous petrology, geochemistry and mineral resources.

This book is the collection of papers from the latest International Uranium Mining and Hydrogeology Conference (UMH VII) held in September 2014, in Freiberg, Germany. It is divided to five sessions: Uranium Mining, Uranium and Phosphates, Clean-up technologies for water and soil. Uranium and daughter nuclides and basic research and modeling. Each session covers a wide range of related topic and provides readers with up to date research and solutions on those matters.

This book gives practical advice and ready to use tips on the design and construction of subsurface reservoir models. The design elements cover rock architecture, petrophysical property modelling, multi-scale data integration, upscaling and uncertainty analysis. Philip Ringrose and Mark Bentley share their experience, gained from over a hundred reservoir modelling studies in 25 countries covering clastic, carbonate and fractured reservoir types. The intimate relationship between geology and fluid flow is explored throughout, showing how the impact of fluid type, production mechanism and the subtleties of single- and multi-phase flow combine to influence reservoir model design. Audience: The main audience for this book is the community of applied geoscientists and engineers involved in the development and use of subsurface fluid resources. The book is suitable for a range of Master's level courses in reservoir characterisation, modelling and engineering. * Provides practical advice and guidelines for users of 3D reservoir modelling packages * Gives advice on reservoir model design for the growing world-wide activity in subsurface reservoir modelling * Covers rock modelling, property modelling, upscaling and uncertainty handling * Encompasses clastic, carbonate and fractured reservoirs

Crystals are everywhere, from natural crystals (minerals) through the semiconductors and magnetic materials in electronic devices and computers or piezoelectric resonators at the heart of our quartz watches to electro-optical devices. Understanding them in depth is essential both for pure research and for their applications. This book provides a clear, thorough presentation of their symmetry, both at the microscopic space-group level and the macroscopic point-group level. The implications of the symmetry of crystals for their physical properties are then presented, together with their mathematical description in terms of tensors. The conditions on the symmetry of a crystal for a given property to exist then become clear, as does the symmetry of the property. The geometrical representation of tensor quantities or properties is presented, and its use in determining important relationships emphasized. An original feature of this book is that most chapters include exercises with complete solutions. This allows readers to test and improve their understanding of the material. The intended readership includes undergraduate and graduate students in materials science and materials-related aspects of electrical and optical engineering; researchers involved in the investigation of the physical properties of crystals and the design of applications based on crystal properties such as piezoelectricity, electro-optics, optical activity and all those involved in the characterization of the structural properties of materials.

This series presents critical reviews of the present position and future trends in modern chemical research. The short and concise reports on chemistry are each written by world renowned experts. This series is still valid and useful after 5 or 10 years. More information as well as the electronic version of the whole content available at: springerlink.com.

The book presents the results from the Uranium Mining and Hydrogeology Conference (UMH VI) held in September 2011, in Freiberg, Germany. The following subjects are emphasised: Uranium Mining, Phosphate Mining and Uranium recovery. Cleaning up technologies for water and soil. Analysis and sensor for Uranium and Radon and Modelling.

Fluid-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.

The Earth's rocky mantle convects to lose heat, which comes from the liquid iron core below. The mantle's interfaces - the core-mantle boundary, and the lithosphere - may hold the key to understanding mantle motion because of the seismic anisotropy present in these parts of the Earth. In this thesis, Andy Nowacki presents a precise but comprehensive review of the current state of the art in studying flow with anisotropy, mineral physics and geodynamics. New measurements of shear wave anisotropy in the lowermost mantle and at mid-ocean ridges are used to constrain mechanisms of creep and melt extraction in the mantle. A model of global flow is used to predict anisotropy in the deep Earth, and novel methods to forward model shear wave splitting are described. Future studies of mantle flow must incorporate the understanding gained in this thesis. The thesis contains a substantive introduction to the structure of the Earth, seismic anisotropy in general and in the core-mantle boundary region, and mid-ocean ridge processes. It also describes novel methods for forward modelling and interpreting shear wave splitting data. Three chapters present timely research into dynamics at divergent plate boundaries and at the core-mantle boundary.

The book contains the Proceedings of the 37th International Symposium on Archaeometry, 12th May 2008, Siena, Italy. The aim of the Symposium is to promote the development and use of scientific techniques in order to extract archaeological and historical information from cultural heritage and the paleoenvironment. It involves all Natural Sciences and all types of objects and materials related with human activity. Papers deal with the development and/or application of scientific techniques for extracting information related to human activities of the past, including the biological nature of man himself and the environment in which he lived. Topics include: Field Archaeology and Intergrated Site Studies; Archaeo-chronometry including recent developments in Radiocarbon Dating; Human - Environment Interactions including Geoarchaeology, Palaeoclimate studies, Landscape Archaeology, Environmental reconstructions, etc.; Bioarchaeology; Food preparation and consumption in Antiquity; the Technology and Provenance of Stone, Plaster, Pigments;Ceramics, Glazes, Glass and Vitreous Materials, Metals and Metallurgical Ceramics; and Micro/nano diagnostic techniques.

This book provides information on the distribution of the available energy resources throughout the continent and how it is linked to the development of individual states. Africa is considered one of the poorest continents in the world, mainly because its development has historically depended on imported resources including technical expertise. This view and its associated resource management strategy are based on the perception that Africa lacks sufficient energy resources to drive its development agenda. Analyses of individual countries' energy potentials, exploitation levels and distribution mechanisms are provided with a view to identifying additional factors that are stifling Africa's economic development. One critical factor is the relationship between available energy resources and the energy mixes chosen by different states, and how these can be exploited to produce the right blend of energy for various applications such as industrial, transport, domestic, and recreational uses. The authors provide an in-depth analysis of the advantages and disadvantages of different energy sources in terms of their environmental, industrialization and distribution costs, impacts, and the development options best suited for improving Africa's economic situation. This analysis is based on the assertion that Africa is indeed blessed with abundant energy resources, which have not been effectively exploited. The book not only reviews Africa's energy situation in general, but also reveals that, while there are certainly circumstances peculiar to individual countries, the similarities, especially within Sub-Saharan African countries, outweigh the differences. That being said, the challenges and available opportunities in each country should be viewed with due consideration given to the prevailing national resource management environment. Many initiatives in Africa fail because of the many loopholes in the management structures, which allow corruption, theft, and mere selfishness to thrive. In addition to the negative impacts of these factors on implementation activities, there is also a general lack of institutional support for initiatives that could otherwise be very progressive. Thus, taken together, these retrogressive practices stifle African energy development plans. The book offers a valuable guide for developers, investors, researchers and environmentalist, providing in-depth insights on the relationship between available energy resources and development trends in Africa. "By harnessing the wind and sun, your vast geothermal energy and rivers for hydropower, you can turn this climate threat into an economic opportunity." US President Obama's address to the African Union (2015)

This book will broaden readers' understanding of pegmatites in a special geodynamic setting, dealing with the emplacement of the Hagendorf-Pleystein Pegmatite Province (HPPP) in the Central European Variscides. This treatise illustrates the complex processes leading to the formation and partial destruction of the pegmatites, documenting the geochronological, chemical, mineralogical, geological and geomorphological / sedimentological data set. The book starts with a detailed account of the economic geology of the various pegmatites, explaining why these deposits are a major resource of ceramic raw materials. In its concluding section, a model of the pegmatite evolution in an ensialic orogen provides meaningful insights into the genetic aspects of pegmatite generation. The Late Paleozoic rare-element pegmatites of the HPPP, Oberpfalz-SE, Germany, rank among the largest concentrations in Europe. The biggest pegmatite of this mining district totals 4.4 million tons of ore (Hagendorf-South). The mining history of the HPPP is restricted to the 20th century, when local entrepreneurs started mining operations in search of ceramic raw materials, feldspar and quartz. Today the "Silbergrube Aplite" is still worked for feldspar. The traditional mining of pegmatitic and aplitic rocks in Central Europe, such as the Bohemian Massif, which is shared by Germany, the Czech Republic, Poland and Austria, has been focused on these industrial minerals. In addition to these major commodities, lithium was mined for a period of time. But even today many of these pegmatites of calc-alkaline affiliation have not lost their appeal to mineralogists and mineral enthusiasts for their wealth of minerals that contain P, Nb, Ta, Li, Be, B, U, Th, Sc, Ti and Sn. The most favorable crustal section to bring about pegmatitic rocks of this type, encompassing pegmatoids, metapegmatites, reactivated pseudopegmatites and pegmatites sensu stricto is the ensialic orogen, exemplified by the Variscan (Hercynian) Orogen, which geodynamically connects the Paleozoic pegmatite provinces in North America and Europe. The geological history of the HPPP, however, goes much further than the Carboniferous-Permian magmatic activity, when the last structural disturbances of the Variscan orogeny affected the NE-Bavarian Basement between 450 and 330 Ma. During this time mafic magmatic rocks together with calcareous and arenaceous sediments were converted into paragneisses, calcsilicate rocks, and amphibolites. It is the period of time when tectonic shortening led to over thrusting and when the emplacement of nappes and the architectural elements of the ensialic orogen began taking shape. During the Late Permian, the Mesozoic and the Cenozoic, the HPPP did not lie idle in geological terms; hypogene and supergene alteration continued and found its most recent expression in alluvial-fluvial "nigrine" placer deposits, which resulted from the unroofing of the pegmatites and aplites in the HPPP and can be used even outside HPPP as an ore guide to pegmatites.

1 Analysenmethoden.- 1.1 Anwendung der Sektorfeld-ICP-MS zur Bestimmung der Hintergrundbelastung der Bevoelkerung mit Platinmetallen.- 1.2 Voltammetrische Bestimmung von Platin- und Rhodiumspuren in Umweltkompartimenten und biologischen Materialien.- 1.3 Platin-Speziation in pflanzlichen Materialien mittels HPLC-ICP-MS.- 1.4 Platin Speziesanalytik mit Hilfe der on-line Kopplung von Kapillarelektrophorese und ICP-MS: Entwicklung, Vorteile und Anwendung dieser schnellen und nachweisstarken Methode.- 1.5 Bestimmung von Palladium in Umweltkompartimenten.- 1.6 Bestimmung von Palladium in biologischen Proben.- 1.7 Trennverfahren fur Platin-Spezies.- 1.8 Trennungen der Metalle der Platingruppe (PGE) mit HPLC und Vergleich mehrerer Probenvorbereitungstechniken.- 1.9 Anwendung der Nickelsulfid-Dokimasie zur Bestimmung von Platingruppenelementen (PGE) in Umweltmaterialien mittels Graphitrohr-AAS.- 2 Stand der Katalysator-Technik.- 2.1 Schadstoff-Verminderung in Kfz-Abgasen durch Regelung des Kraftstoff-Gemisches mit der Lambda-Abgas-Sonde.- 2.2 Quantitative Motorstand-Reihenuntersuchungen zur Bestimmung der Platinemissionen aus Automobilabgaskatalysatoren.- 3 Piatin(metalle) in Umweltkompartimenten.- 3.1 Platinkonzentrationen in Staubproben aus Frankfurt am Main und Umgebung.- 3.2 Verteilung und Konzentrationen von Platin, Palladium und Rhodium in Umweltmaterialien entlang der Bundesautobahn A 5 (Akm 459 - Akm 524).- 3.3 PGE-Konzentrationen in Boeden entlang der Autobahnen A 45 und A 3 im Vergleich zu Boeden im Einflussbereich der edelmetallverarbeitenden Industrie in Hanau.- 3.4 Platin in kommunalen Klaranlagen.- 3.5 Biomonitoring verkehrsbedingter Platin-Immissionen.- 3.6 Relevanz von Platinemissionen durch Krankenhauser.- 3.7 Verteilung und Konzentration von Platingruppenelementen (PGE) im Boden entlang der Autobahn Frankfurt-Mannheim.- 4 Bioverfugbarkeit von Platin(metallen).- 4.1 Automobilverkehr und Stoerungen im Wasserhaushalt von Pflanzen.- 4.2 Pflanzenverfugbarkeit, Boden - Pflanze Transfer.- 4.3 Zum Transformationsverhalten Kfz-emittierten Platins in einem Boden und Platinaufnahme durch Pflanzen.- 4.4 Zur Loeslichkeit und Speziestransformation von Platin aus Autoabgaskatalysatoren durch Huminsaure.- 4.5 Geochemisches Verhalten von Platinmetallen aus Autoabgaskatalysatoren in Sedimenten und im Wasser aus einem Versickerbecken.- 5 Toxikologisches und allergologisches Gefahrdungspotential von Platin und anderen Platinmetallen (Arbeitsmedizin).- 5.1 Toxikologisches Gefahrdungspotential der Platingruppenelemente Platin, Palladium und Rhodium.- 5.2 Arbeitsmedizinische Aspekte der Platinsalzallergie: Krankheitsbild, Diagnostik, Prognose, Pravention und Therapie.- 5.3 Abschatzung des Gesundheitsrisikos von Platinemissionen aus Automobilabgaskatalysatoren.- 5.4 Biomonitoring von Platin im Urin in der Arbeitsmedizin.

The goal of this Third Edition is to update long-term data presented in earlier editions and to generate new syntheses and conclusions about the biogeochemistry of the Hubbard Brook Valley based on these longer-term data. There have been many changes, revelations, and exciting new insights generated from the longer data records. For example, the impact of acid rain peaked during the period of the HBES and is now declining. The longer-term data also posed challenges in that very marked changes in fluxes occurred in some components, such as hydrogen ion and sulfate deposition, calcium and nitrate export in stream water and biomass accumulation, during the almost 50 years of record. Thus, presenting "mean" or "average" conditions for many components for such a long period, when change was so prominent, do not make sense. In some cases, pentads or decades of time are compared to show these changes in a more smoothed and rational way for this long period. In some cases, a single period, often during periods of rapid change, such as acidification, is used to illustrate the main point(s). And, for some elements a unique mass balance approach, allowing the calculation of the Net Ecosystem Flux (NEF), is shown on an annual basis throughout the study.

F. Jerry Lucia, working in America's main oil-rich state, has produced a work that goes after one of the holy grails of oil prospecting. One main target in petroleum recovery is the description of the three-dimensional distribution of petrophysical properties on the interwell scale in carbonate reservoirs. Doing so would improve performance predictions by means of fluid-flow computer simulations. Lucia's book focuses on the improvement of geological, petrophysical, and geostatistical methods, describes the basic petrophysical properties, important geology parameters, and rock fabrics from cores, and discusses their spatial distribution. A closing chapter deals with reservoir models as an input into flow simulators.

This practical step-by-step guide describes the key geological field techniques needed by today's exploration geologists involved in the search for metallic deposits. The techniques described are fundamental to the collection, storage and presentation of geological data and their use to locate ore. This book explains the various tasks which the exploration geologist is asked to perform in the sequence in which they might be employed in an actual exploration project. Hints and tips are give. The steps are illustrated with numerous examples drawn from real projects on which the author has worked. The book emphasizes traditional skills and shows how they can be combined effectively with modern technological approaches.

This book is not designed to be an exhaustive work on mine wastes. It aims to serve undergraduate students who wish to gain an overview and an understanding of wastes produced in the mineral industry. An introductory textbook addressing the science of such wastes is not available to students despite the importance of the mineral industry as a resource, wealth and job provider. Also, the growing imp- tance of the topics mine wastes, mine site pollution and mine site rehabilitation in universities, research organizations and industry requires a textbook suitable for undergraduate students. Until recently, undergraduate earth science courses tended to follow rather classical lines, focused on the teaching of palaeontology, cryst- lography, mineralogy, petrology, stratigraphy, sedimentology, structural geology, and ore deposit geology. However, today and in the future, earth science teachers and students also need to be familiar with other subject areas. In particular, earth science curriculums need to address land and water degradation as well as rehabili- tion issues. These topics are becoming more important to society, and an increasing number of earth science students are pursuing career paths in this sector. Mine site rehabilitation and mine waste science are examples of newly emerging disciplines. This book has arisen out of teaching mine waste science to undergraduate and graduate science students and the frustration at having no appropriate text which documents the scienti?c fundamentals of such wastes.

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.

Clay Sedimentology is a comprehensive textbook divided into six parts: - clay minerals and weathering - clay sedimentation on land - origin and behaviour of clay minerals and associated minerals in transitional environments (estuaries, deltas) and shallow-sea environments - diverse origins of clay in the marine environment - post-sedimentary processes intervening during early and late diagenesis - use of clay stratigraphic data for the reconstruction of past climate, marine circulation, tectonics, and other paleogeographical aspects. A basic idea on most topics dealing with sedimentary clays is presented and controversial data and uncertainties from the frontiers of knowledge are discussed.

Barrier islands represent a complex coastal system that includes a number of different sedimentary depositional environments; nearshore zone, beach, dunes, washover fans, marshes, tidal flats, estuaries, lagoons, and tidal inlets. The morphodynamics of these fragile coastal systems provide a further complication to this coastal type. Although barrier islands comprise only 15% of the world's coastline, they have received a far greater proportion of attention from the scientific and engineering community, and more recently, from coastal managers and environmentalists. Modern barrier islands are arguably the most expensive and most vulnerable of all coastal environments. Pressure from developers for residential, industrial, and recreational development has caused most of our barriers to become significantly impacted by human activity, especially over the past few decades. These pres sures have led to extensive preservation of natural barriers through efforts from all levels of government and also by private organizations. Governments have also formed coastal management programs that help to control any future de velopment with the intent being to keep human activity compatible with barrier island morphodynamics. In order to devise appropriate coastal zone management programs, it is necessary to have a comprehensive understanding of the morpho dynamics of barrier island systems. This volume provides comprehensive details on barrier island morphology, sediment distribution, and the process-response mechanisms that cause changes to both. These are the important aspects of barrier systems that can provide important input into the development and implementation of coastal management programs."

Jean-Francois Daubuisson (1769 1841), geologist and engineer, was an Officer of the Legion d'Honneur, Knight of St Louis and Chief Engineer at the Royal Mining Corps. He published numerous papers on geology, mining and hydraulics, and is best known for his textbooks, Traite de Geognosie and Traite d'Hydraulique. He studied geology and mineralogy in Freiburg with Abraham Werner, the key proponent of Neptunism, the theory that all rocks had an aqueous origin. Later in his career Daubuisson was to side with the Plutonists, who argued that basalts formed from molten rock. However, in this paper, published in French in 1803, he describes his observations of the basalts of Saxony and argues that they, and all basalts, are sedimentary. This English translation by the Secretary of the Wernerian Natural History Society was published in 1814, and provides a fascinating insight into this discredited but once influential theory of the Earth.