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Influence of Abyssal Circulation on Sedimentary Accumulations in Space and Time
Clays and Clay Minerals of Japan
Man's understanding of how this planet is put together and how it evolved has changed radically during the last 30 years. This great revolution in geology - now usually subsumed under the concept of Plate Tectonics - brought the realization that convection within the Earth is responsible for the origin of today's ocean basins and conti nents, and that the grand features of the Earth's surface are the product of ongoing large-scale horizontal motions. Some of these notions were put forward earlier in this century (by A. Wegener, in 1912, and by A. Holmes, in 1929), but most of the new ideas were an outgrowth of the study of the ocean floor after World War II. In its impact on the earth sciences, the plate tectonics revolution is comparable to the upheaval wrought by the ideas of Charles Darwin (1809-1882), which started the intense discussion on the evolution of the biospere that has recently heated up again. Darwin drew his inspiration from observations on island life made during the voyage of the Beagle (1831-1836), and his work gave strong impetus to the first global oceanographic expedition, the voyage of HMS Challenger (1872- 1876). Ever since, oceanographic research has been intimately associ ated with fundamental advances in the knowledge of Earth. This should come as no surprise. After all, our planet's surface is mostly ocean.
Deep-water (below wave base) processes, although generallyhidden from view, shape the sedimentary record of more than 65% ofthe Earth’s surface, including large parts of ancientmountain belts. This book aims to inform advanced-levelundergraduate and postgraduate students, and professional Earthscientists with interests in physical oceanography and hydrocarbonexploration and production, about many of the important physicalaspects of deep-water (mainly deep-marine) systems. The authorsconsider transport and deposition in the deep sea, trace-fossilassemblages, and facies stacking patterns as an archive of theunderlying controls on deposit architecture (e.g., seismicity,climate change, autocyclicity). Topics include modern and ancientdeep-water sedimentary environments, tectonic settings, and howbasinal and extra-basinal processes generate the typicalcharacteristics of basin slopes, submarine canyons, contouritemounds and drifts, submarine fans, basin floors and abyssalplains.
In the last few years, the quantity of books and papers on the political, economic and legal problems of the exploration and use of the sea and marine resources has considerably increased. But the status and activities of intern a tional organizations related to maritime shipping, fisheries, scientific research in the World Ocean and the protection of the marine environment have not yet, as a whole, been represented in the scientific and reference literature. It would be fair, though, to mention that some general information on marine international organizations may be found in the Yearbook of International Organizations, Brussels, 1979; in Annotated Acronyms and Abbreviations of Marine Science Related International Organizations, U. S. Department of Commerce, 1976; and in the UN Annotated Directory ofIntergovernmental Organizations Concerned with Ocean Affairs, 1976. Voluminous informa tion on organizations engaged in problems of the exploration and use ofthe sea is given in International Marine Organizations by the well-known Polish scientists Lopuski and Symonides, 1978. Meanwhile the increasing volume of practical work related to the participa tion of governmental and scientific bodies as well as individual scientists and specialists in these organizations, the necessity of long-term planning in this field, and the perspectives of the development of these organizations, make necessary a special publication depicting the structure and many-sided activi ties of such international bodies. This book is the first one in which the most complete information on the main marine international organizations is presented.
We wrote Sedimentology of Shale primarily because we lacked a handy, reasonably comprehensive source of information and ideas about shales for students in our sedimentology program. It was also our feeling that the time for shales to receive more study had finally arrived. Sedimentology of Shale also seems very timely because today more sedimentologists are interested in shales. Certainly in the last five years the pace of shale research has no ticeably quickened because the role of shales as important sources of oil, gas, heavy metals and as a long understudied part of the earth's geologic his tory has been recognized. Noteworthy developments include the elucida tion of the importance of trace fossils in shales, the discovery of thick sequences of overpressured shales in regions such as the Gulf Coast (which have important implications for hydrocarbon migration and faulting), the ex tension of the principles of metamorphic facies to the realm of low tempera ture diagenesis by study of the organic matter in shales, and shales as ul timate sources for mineral deposits. Accordingly, we decided it was timely to write a book on shales. In one respect, however, ours is an unusual book. Most books in geology are produced after one or two decades of progress have been made in a field and attempt to summarize and evaluate that progress.