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Miocene carbonates are a rich but largely untapped source for general models of carbonate stratigraphy, paleoecology, diagenesis and hydrocarbon exploration. Lower and Middle Miocene reef carbonates display an ample worldwide distribution (Fig. 1A), surpassing the modern reef belt (Fig. 1B). In contrast, Upper Miocene reefs are remarkably restricted (Fig. 1C), reflecting the well-known global-cooling trend during Miocene times. The Mediterranean regions, which we define to include the entire Mediterranean Sea plus the Paratethys, Red Sea and nearby Atlantic areas, include a wide variety of Miocene carbonates and some of the world's best outcrops.
Recent years have seen increasing rigour being applied in many industrialised countries to the regulation of industrial emissions and to the quality of water, air, food and soil. This welcome official concern with the quality of the human habitat will, through the regular monitoring of environmental media that it implies, have important consequences for the training of professional environmental scientists. Monitoring agencies will require more analysts familiar with the special obstacles that compositionally diverse environmental materials can put in the path of reliable analysis. Professionals who interpret such analyses, too, though they may not be trained in the the technicalities of geochemical analysis, will need to recognise the limitations of the analytical methods employed and understand the quality control mechanisms upon which the industry depends, if they are to draw objective and reliable conclusions from their data.
TYSON, R. V. & PEARSON, T. H. Modern and ancient continental shelf anoxia: an overview Modern shelf anoxia BOESCH, D. F. & RABALAIS, N. N. Effects of hypoxia on continental shelf benthos: comparisons between the New York Bight and the Northern Gulf of Mexico RABALAIS, N. N., TURNER, R. E., WISEMAN, W. I. Jr. & BOESCH, D. F. A brief summary of hypoxia on the northern Gulf of Mexico continental shelf: 1985-1988 HARPER, D. E. Jr., MCKINNEY, L.D., NANCE, J. M. & SALTER, R. R. Recovery responses of two benthic assemblages following an acute hypoxic event on the Texas continental shelf, northwestern Gulf of Mexico VAN DER ZWAAN, G. J. & JORISSEN, F. J. Biofacial patterns in river-induced shelf anoxia
Biogeochemistry is becoming an increasingly popular subject in graduate education. Courses in ecology, geography, biology, chemistry, environmental science, public health, and environmental engineering all have to include biogeochemistry in their syllabuses to a greater or lesser extent. Humanity’s ever growing impact on the Environment, and the consequent local, regional, and global effect demand a profound understanding of the mechanisms underlying the sustainability of the biosphere and its compounds. The ideas of biogeochemistry about the universality of biogeochemical cycles involving the mass exchange of chemical elements between living organisms and the environment in the Earth’s surface appear to be quite productive in this high priority academic and scientific discipline. In biogeochemical cycling the active principles come from biota which global biological and geological activity alter slowly the biosphere’s compartments. On the other hand, the environment causes the living organisms evolve.
This is a book about enhancing natural gas production using one of the most important and widespread well completion technologies — hydraulic fracturing. The book addresses the way that natural gas is produced from natural reservoirs (Chapter 2) and then describes diagnostic techniques that can pinpoint whether the well is producing as it should or whether intervention should be undertaken (Chapter 3), which is the central theme of this book. Hydraulic fracturing is introduced as the solution of choice, showing the idiosyncratic nature of natural gas wells compared to oil wells (Chapter 4).
Spectroscopy is the study of the interaction of electromagnetic radiation with the matter. There are three aspects of the spectroscopic measurement: irradiation of a sample with electromagnetic radiation; measurement of the absorption, spontaneous emission and scattering (Rayleigh elastic scattering, Raman inelastic scattering) from the sample; and analysis and interpretation of these measurements. The main subject of our book is spontaneous luminescence of natural minerals. We have used the term luminescence, which is the general term of the phenomenon. Luminescence may be subdivided to the fast fluorescence with spin-allowed transition and slow phosphorescence with spin-forbidden transition. Afterglow may be added, which is related to emission after trapping of an electron elsewhere. <...>
This book presents nine chapters of technical knowledge about pressure transient analysis. All of the chapters cover different subjects and provide the reader with a complete understanding of the well testing methodology and analysis, enabling well test engineers to comprehend the interpretation process together with the procedures required for reservoir interpretation.
The fossils of the Miocene beds of New Jersey, like those of the Cretaceous and Eocene beds, have never until now been systematically studied or recorded. Many of them which are as yet peculiar to the deposits of the State have, however, been described haphazard, as it were, by different writers, with scarcely any other object in view than that of describing the species which happened to fall into their hands. In this way a few of the most prominent forms have become known, but very few species are mentioned in any of.the lists of Miocene fossils as pertaining to the New Jersey fauna.