Rutley's elements of mineralogy has been around for a long time, certainly throughout my own lifetime; and if my great grandfather had read geology, it would have been prescribed reading for him too It has been rewritten and revised frequently since fir t conceived by Frank Rutley in the late 19th century. Major revisions occurred in 1902, and then in 1914, when H. H. Read first took over the authorship, and thereafter in 1936 and in 1965 when the last major changes occurred. It was with some trepidation that I agreed to attempt this revision. I had been asked to do it by Janet Watson in 1979, but various commitments delayed my start on it until 1984. This 27th edition encompasses a number of changes. Chapters 1-5 have the same headings as before, but considerable changes have been made in all of them, particularly 1, 3, 4 and 5. Comments sought prior to the revision revealed considerable disagreement about the role of blowpipe analyses in the book. I have only once had blowpipe analyses demon strated to me, and have never used them; but there is no doubt that they are employed in many countries, and many of the tests (flame colour, bead, etc. ) are still useful as rapid indicators of which element is present in a mineral. I have therefore kept blowpipe analysis information in Rutley, but have relegated it to an appendix."

The past decade has seen remarkable growth in research related to petroleum reseIVoir simulation. This growth reflects several developments, not the least of which is the increased interest in oil recovery technologies requiring sophisticated engineer ing. Augmenting this interest has been the broader availability of supercomputers capable of handling the tremendous computational demands of a typical reseIVoir simulator. The field of reseIVoir simulation incorporates several major facets of applied mathematics. First, in view of the varieyt and complexity of the processes encoun tered, it is imperative that the modeler adopt a systematic approach to establishing the equations governing reseIVoir flows. Second, the mathematical structure of these flow equations needs to be carefully analyzed in order to develop appropriate and efficient numerical methods for their solution. Third, since some aspects of the discretized flow equations are typically stiff, one must develop efficient schemes for solving large sparse systems of linear equations. This monograph has three parts, each devoted to one of these three aspects of reseIVoir modeling. The text grew out of a set of lectures presented by the authors in the autumn of 1986 at the IBM Scientific Center in Bergen, Norway. We feel that it is only appropriate to caution the reader that many of the ideas that we present in this monograph do not reflect standard approaches in petroleum reseIVoir simulation. In fact, our aim is to outline promising new ways of attacking reseIVoir simulation prob lems, rather than to compile another textbook for the mainstream."

"International Mineral Economics" provides an integrated overview of the concepts important for mineral exploration, mine valuation, mineral market analysis, and international mineral policies. The treatment is interdisciplinary, drawing on the fields of economics, geology, business, and mining engineering. Part I, Economic Geology and Mineral Development, examines the "technical" concepts important for understanding the geology of ore deposits, the methods of exploration and deposit evaluation, and the activities of mining and mineral processing. Part II, Mineral Economics, focuses on the "economic" and related concepts important for understanding mineral development, the evaluation of exploration and mining projects, and mineral markets and market models. Finally, Part III, International Mineral Policies, reviews and traces the historical development of the policies of international organizations, the industrialized countries, and the developing countries.

The book deals with natural climate variations during the last 600,000 years. Among the topics astronomical influence on paleoclimates, climate and environment, natural CO2-variants based on investigations of ice curves and climatic information from wood density are the most important. This long and short term variability is the base for modelling and prediction of anthropogenically induced climatic changes.

Within the last decade or so, the accelerated growth of Nigeria in the fields of urbanisation, population, business as well as industry has led to some attention in assessment of available water resources in various parts of the country. Many workers (du Preez and Barber, 1965; Jackson, 1978; Faniran and Omorinbola, 1980; Ofodile, 1983; Egboka, 1983; Akujieze, 1984; Ogbukagu, 1984; Uma, 1984) have made significant contributions in this area. Water is important because the attainment of the goals of any society as well as the health and well-being of the population depends on a plentiful and reliable supply of this natural resource. Water forms an indispensable input into economic activities such as commerce, tourism and industry. The results of the various researches have revealed that water resources (surface and groundwater) in many parts of the country, especially the southern part, are more than adequate to meet any demand and only need development. A complete appraisal of available water resources is often best accomplished when aspects of water quality are included. This is because in a planned water supply system, quality constraints and requirements dictate the sources of water allocated to various stages. A public water supply, though contributing greatly to the human health and well-being, can also be a vehicle for spreading disease if not properly handled. In this paper, water quality of selected water resources (surface and groundwater) in some parts of Imo State, Nigeria are reported and suggestions advanced for their healthy untilization.

Characteristic examples of evaporite basins, mostly of moderate size, are discussed in terms of type (playas, continental sabkhas, barred basins), deposits, fossils, relics and pseudomorphs of gypsum found, and complex of diagenesis, e.g. in the Red Sea Miocene where reef complexes predate the deposition of massive evaporites. Two models, the sabkha model and the deep desiccation basin model, are both employed to explain the formation of "evaporite basins." In many cases both models must be combined as many evaporites were formed in subaqueous environments.

This sourcebook to the prodigious literature on applications of computers and statistics to geology contains over 2000 references. The glossary provides succinct explanations of most statistical and mathematical terms. Computer topics include hardware, software, programming languages, databases, and communications graphics, CAO/CAM, CAI, GIS and expert systems. Statistical topics range from elementary properties of numbers through univariate, bivariate to multivariate methods. The brief notes on each method provide a general guide to what the technique does, and are illustrated with worked examples from a wide range of geological disciplines. Students and researchers will find the book useful in coping with the explosion of information which has taken place in geology, and to make the best possible use of computers in interpreting acquired data.

This book reports new developments in research on the Zechstein basin which is one of the classical saline giants. Recently much information was gathered which changes earlier ideas on the deposition and diagenesis of the Zechstein basin.

Discusses the global evolution of the earth, such as core- mantle separation, mantle-crust evolution, origin of ocean- atmosphere system, on the basis of isotope earth science and paleomagnetism, where recent devlopment in planetology and astrophysical theories are extensively taken into account.

Aquatic chemistry is becoming both a rewarding and substantial area of inquiry and is drawing many prominent scientists to its fold. Its literature has changed from a compilation of compositional tables to studies of the chemical reactions occurring within the aquatic environments. But more than this is the recognition that human society in part is determining the nature of aquatic systems. Since rivers deliver to the world ocean most of its dissolved and particulate components, the interactions of these two sets of waters determine the vitality of our coastal waters. This significant vol ume provides not only an introduction to the dynamics of aquatic chem istries but also identifies those materials that jeopardize the resources of both the marine and fluvial domains. Its very title provides its emphasis but clearly not its breadth in considering natural processes. The book will be of great value to those environmental scientists who are dedicated to keeping the resources of the hydrosphere renewable. As the size of the world population becomes larger in the near future and as the uses of materials and energy show parallel increases, the rivers and oceans must be considered as a resource to accept some of the wastes of society. The ability of these waters and the sediments below them to accommodate wastes must be assessed continually. The key questions relate to the capacities of aqueous systems to carry one or more pollutants."

The first edition of this book was published in 1965 and its French translation in 1966. The revised second edition followed in 1967 and its Russian translation became available in 1969. Since then, many new petrographic observations and experimental data elucidat- ing reactions in metamorphic rocks have made a new approach in the study of metamorphic transformation desirable and possible. It is felt that this new approach, attempted in this book, leads to a better unders- tanding of rock metamorphism. The concept of metamorphic facies and subfacies considers asso- ciations of mineral assemblages from diverse bulk compositions as characteristic of a certain pressure-temperature range. As new petrographic observations accumulated, it became increasingly difficult to accommodate this information within a manageable framework of metamorphic facies and subfacies. Instead, it turned out that mineral assemblages due to reactions in common rocks of a particular composi- tion provide suitable indicators of metamorphic conditions. Metamorphic zones, defined on the basis of mineral reactions, very effectively display the evolution of metamorphic rocks. Thus the im- portance of reactions in metamorphic rocks is emphasized. Experimen- tal calibration of mineral reactions makes it possible to distinguish reac- tions which are of petrogenetic significance from those which are not. This distinction provides guidance in petrographic investigations un- dertaken with the object of deducing the physical conditions of metamorphism.

Das Motiv fur die Veranstaltung dieses Symposiums uber die Beziehungen zwischen metallogenetischen und geochemischen Provinzen war ein egoistisches Informationsbedurfnis des Organisators. Als ich 1967 an dem Manuskript uber Erzprovinzen und Kontinentaldrift arbeitete, ergab sich die Frage, ob die Metalle der Lagerstatten in den wandernden Kontinentalschollen beheimatet sind oder ob sie aus dem wechselnden Substratum des oberen Mantels und der daraus ge- speisten ozeanischen Kruste stammen. Es galt also, das Material zu uberprufen, das die Beziehungen der Erzlagerstatten zur Geochemie ihrer kontinentalen Um- gebung oder zur Geochemie des Ozeanbodens zeigt. Dies kann zugleich auch Bei- trage ergeben zu dem Problem der modernen Iateralsekretionaren Lagerstatten- bildung. Die wirkungsvollste Art, sich bei der heutigen grossen Menge von Literatur uber ein komplexes Thema zu informieren, ist, kompetente Leute zusammenzu- bitten, damit sie daruber vortragen und diskutieren. Ich darf sagen, dass meinem Bedurfnis voll Genuge geleistet wurde und ich habe dafur all den lieben Kolle- gen, die zum Teil von sehr weit nach Leoben gekommen sind, herzlichen Dank zu sagen. Alle Vortrage behandeln, ja man kann fast sagen, klaren in ihrer Gesamt- heit das aufgeworfene Problem. Ich mochte aber doch glauben und hoffen, dass nicht nur der Veranstalter, son- dern auch die Teilnehmer von den Vortragen und Diskussionen Nutzen hatten. Ein intensiver Gedankenaustausch war moglich, da die Teilnehmerzahl mit Ab- sicht klein gehalten und auf spezielle Sad1kenner beschrankt war und da das Programm im Gegensatz zu vielen Kongressen weite Lucken fur Diskussionen liess.

This student-oriented text is written in a casual, jargon-free style to present a modern introduction to mineralogy. It emphasizes real-world applications and the history and human side of mineralogy. This book approaches the subject by explaining the larger, understandable topics first, and then explaining why the "little things" are important for understanding the larger picture.

The monograph offers a comprehensive discussion of the role of evaporites in hydrocarbon generation and trapping, and new information on low temperature and high temperature ores. It also provides a wealth of information on exploitable salts, in a comprehensive volume has been assembled and organized to provide quick access to relevant information on all matters related to evaporites and associated brines. In addition, there are summaries of evaporite karst hazards, exploitative methods and problems that can arise in dealing with evaporites in conventional and solution mining. This second edition has been revised and extended, with three new chapters focusing on ore minerals in different temperature settings and a chapter on meta-evaporites. Written by a field specialist in research and exploration, the book presents a comprehensive overview of the realms of low- and high-temperature evaporite evolution. It is aimed at earth science professionals, sedimentologists, oil and gas explorers, mining geologists as well as environmental geologists.

A fascinating exploration of exquisite images captured from natural materials, and of their applications in fashion, environmental design, and apps that anticipate a new era of digitally-driven individual creativity. Data From Nature begins with the chance encounter between an ammonite and a digital scanner and goes on to relate the author's growing immersion in the micro-scale beauty of minerals and--thanks to new digital means of production--their applications in wide areas of design. These include an award-winning range of silk scarves for Liberty of London (also sold in Saks Fifth Avenue); "frocks from rocks"; a striking architectural facade in London, and the transformation of his own house and garden using the latest digital techniques. Along the way we learn about how minerals form in the Earth; ways they have been admired and imagined from ancient civilizations to the dawn of Modernity; and discover how the inlaid surfaces of Renaissance cabinets of curiosity could inspire creative coloring and design apps intended to equip children and adults alike to participate creatively in the Digital Revolution. And as if all this weren't enough, the book ends as improbably as it started with a short biography of a "lost" (for which read "fictional") seventeenth-century artist, Carlo Alcite, whose "works" reveal powers of invention and draftsmanship worthy of a baroque master.

Mining is a capital-intensive industry, and involves long lead times to develop projects that demand a structured approach, from mine exploration to exit. This book provides mine developers, investors, owners, shareholders, and mineral policymakers a comprehensive game plan to raise capital for the development of new mining projects or to bolster operational mines. The author, an experienced mining capital consultant, shows how mine developers and mine owners can secure capital in any phase of the commodity price cycle, at any site, and at any project stage. The book follows a proven and structured approach that enables mine developers and owners to successfully raise capital for their projects. With the aid of case studies and practical methods, the reader will learn the essentials on topics ranging from developing and marketing a business case for investment, to the types and sources of mining capital for different project stages, as well as the structure and significance of due diligence. The author presents actual mining projects and their funding plans, transaction structures and term sheets for capital. The mining projects discussed represent various project stages, commodities, and parts of the globe, offering a comprehensive reference guide for mine developers, investors and promoters alike.

Wasser". Dieser MeBfiihler wird nun irgendwo in der Natur installiert, der Beob- achter befindet sich weit entfemt, vor einem Bildschirm sitzend, auf den die MeB- signale iibertragen werden. Es solI festgestellt werden, ob es regnet oder nicht. 1st nun das MeBintervall zu groB eingesteIlt, etwa alle 12 Stunden ein Signal, so kann der Beobachter bei der Information, Nicht-Wasser" keine Aussage dariiber treffen, ob es regnet oder nicht. Da Regen fUr einen konkreten Raurn betrachtet ein Wechsel von "Wasser" und, Nicht-Wasser", eben die diskreten Regentropfen, darsteIlt, ist die Information, Nicht-Wasser" ebenso fiir Regen wie fUr schOnes Wetter richtig, bei Regen eben nur weniger oft. Nach dieser Erfahrung wird das MeBintervaIl nun verkleinert, alle paar Sekun- den erhiUt nun der Beobachter eine Information iiber "Wasser" und, Nicht- Wasser". Und jeden Abend urn halb Sieben bis Sieben Uhr regnet es, zurnindest meldet der Fiihler abwechselnd "Wasser" und, Nicht-Wasser". Des Ratsels Lo- sung: Jeden Abend wird der Garten gesprengt, in dem sich der MeBfiihler befindet. Der Raurn, der vom MeBfiihler erfaBt wird, ist zu klein, urn eindeutig zwischen natiirlichem Regen und anderen sporadischen Wassertropfenereignissen unter- scheiden zu konnen. Fiir einen an den Bildschirm verbannten Beobachter ist die Feststellung, ob es regnet, nur gegeben, wenn mehrere MeBfiihler iiber einen hin- reichend groBen Raum verteilt in entsprechend kurzen Intervallen eine Information dariiber liefem, ob sie gerade vom Wasser oder von Luft umgeben sind. MeBraurn und MeBzeit bestimmen also die durch die Messungen gewonnene Aussage.

The evolution of geological cartography in Cuba in its more than 135 years of history has been possible through the consultation of numerous archival reports, publications, maps and personal interviews with different authors and geologists of vast experience. A brief critical analysis is made of the increase in the degree of geological knowledge of the country since the elaboration of the Geological Sketch of the Cuban Island at a scale of 1: 2 000 000 (Fernandez de Castro, 1883), first of Cuba and of Ibero-America, until the most recent Digital Geological Map of Cuba at scale 1: 100 000 (Perez Aragon, 2016). Cuba and its surroundings are a geological mosaic in the southeast corner of the North American plate with rocks from many different origins, from Proterozoic to Quaternary, extended along the southern border of the plate. From the Eocene, this belt has been dissected by several great faults, related to the development of some great oceanic depressions (Cayman trough and Yucatan basin). The fossil record of Cuba, which covers approximately the last 200 million years of life on Earth, is rich in very varied fossils, witnessing a wide diversity of organisms, both animals and plants, that inhabited the Antillean and Caribbean region; and that constitute the inheritance of the biological diversity that the current Cuban archipelago exhibits. As a result of the preparation of the Cuban Metallogenic Map at scale 1: 250 000, forty-one models and eight sub-models of metallic mineral deposits were identified. These models, of descriptive-genetic type, together with the analysis of their spatial distribution and their relationship with geology, allowed the identification and mapping of ten mineral systems, linked to the geodynamic environments present in the Cuban territory. Cuba has large deposits of limestone, loam, dolomite, kaolin, gypsum and anhydrite, rock salt, marbles, sands and clays of different types, zeolites, peat, therapeutic peloids and many more. There are manifestations of decorative and precious rocks such as jasper, jadeite, different varieties of quartz and even xylopals. A compilation of geochemical data of oceanic basalt samples from previous works, together with data of analyzed samples during this study in order to discuss geochemical criteria based on immobile element (proxies for fractionation indices, alkalinity, mantle flow and subduction addition), provide a comprehensive ophiolite classification according to their tectonic setting. This book addresses different facets of the geological knowledge of Cuba: history of its cartography, marine geology, fossil record, stratigraphy, tectonics, classification of its ophiolites, quaternary deposits, metallogeny and minerageny.

Granites are emblematic rocks developed from a magma that crystallized in the Earth's crust. They ultimately outcrop at the surface of every continent. This book - translated, edited, and updated from the original French edition Petrologie des Granites published by Vuibert in 2011 - gives a modern presentation of granitic rocks, or granites, from magma genesis to their emplacement into the crust and their crystallization. Mineralogical, petrological, physical, and economical aspects are developed in a succession of 14 chapters. Special 'info boxes' discuss topics for those wishing to deepen their knowledge of the subject. Also included is a glossary, a comprehensive bibliography, as well as descriptions of modern techniques. Granites are considered in their geological spatial and temporal frame, in relation with Plate Tectonics and Earth History, and assisted by a large number of high quality illustrations.

The fourth edition of Introduction to Optical Mineralogy has been thoroughly revised and updated to increase reading comprehension and improve the clarity of its illustrations. Author William D. Nesse continues his detailed discussions of the petrographic microscope, the nature and properties of light, and the behavior of light in isotropic and anisotropic minerals, with detailed coverage of uniaxial and biaxial optics. Ideal for advanced undergraduate and graduate courses in optical mineralogy, this accessible text is also an essential resource for petrology and petrography courses.