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'Deep-Sea Sediments' focuses on the sedimentary processes operating within the various modern and ancient deep-sea environments. The chapters track the way of sedimentary particles from continental erosion or production in the marine realm, to transport into the deep sea, to final deposition on the sea floor.
The Earth Science Series of the Circum-Pacific Funding for ship time was made available through Council for Energy and Mineral Resources (CPCEMR) the U. S. Agency for International Development, the is designed to convey the results of geologic research in USGS, the U. S. Office of Naval Research (for RIG's and around the Pacific Basin. Topics of interest include 1982 work), the Australian Development Assistance framework geology, petroleum geology, hard minerals, Bureau, the Australian Bureau of Mineral Resources geothermal energy, environmental geology, volcanology, (BMR) , the New Zealand Ministry of Foreign Affairs, oceanography, tectonics, geophysics, geochemistry, and the New Zealand Department of Scientific and Industrial applications of renewable energy. The CPCEMR sup Research (DSIR), the New Zealand Geological Survey, ports and publishes results of scientific research that will and the New Zealand Oceanographic Institute (NZOI). Coordination of the program was provided by the U. S. advance the knowledge of energy and mineral resource potential in the circum-Pacific region. The Earth Sci Department of State and the South Pacific Applied Geo ence Series is specifically designed to publish papers that science Commission (SOPAC, formerly the United include new data and new maps, report on CPCEMR Nations-sponsored Committee for the Coordination of sponsored symposia and workshops, and describe the Joint Prospecting for Mineral Resources in South Pacific results of onshore and marine geological and geophysical Offshore Areas CCOP/SOPAC) in Fiji. Over 150 scien explorations.
The book is structured thematically, encompassing principles, processes and products, practice and applications. Discussion of processes that control heavy mineral assemblages throughout the rock cycle are presented by leading experts, whose key-note works are followed by specialist case studies. Each work also provides details on the geology of the study area, techniques and data treatment. The high number of contributions represent the collective experience and wisdom of generations of geologists, and provide an invaluable source of references to works carried out in many parts of the world. * Presents a unique and authoritative resource of immediate relevance and practical use to the researcher and applied geologist * Contains case studies demonstrating the broad range of applications of heavy minerals in a variety of modern and ancient geological settings, and in resource exploration * Includes examples of geological problems from employing heavy mineral analysis and establishing criteria that can be applied before deciding to undertake a study
Published by the American Geophysical Union as part of the Special Publications Series. We are pleased to present this edited translation of Oceanic Sedimentation, from the original Russian edition of Alexander Lisitzin's Processes in Oceanic Sedimentation: Lithology and Geochemistry (Nauka). Published originally in 1978, this volume represents an important, major synthesis on oceanic sediments and major processes governing their formation and distribution in space and time. The primary focus of this volume is the influence of the environment, especially climate, on the mineral, chemical, and isotopic composition of sediments and their physical characteristics. This global perspective is rich in data about sediment sources, composition, transportation, volumes, fluxes, and budgets. We consider that this edited translation is of particular importance because Lisitzin's compilation is one of the broadest and most comprehensive available in any language.
There are three types of rock—igneous, metamorphic and sedimentary. Sedimentary rocks form from the weathering, erosion, transportation and deposition of older rocks. Applied Sedimentology describes the formation, transportation and deposition of sediment, and the post-depositional processes that change soft sediment into sedimentary rock. Sedimentary rocks include sandstones, limestones and mudstones. All the world's coal, most of its water and fossil fuels, and many mineral deposits occur in sedimentary rocks. Applied Sedimentology shows how the study of sediments aids the exploration for and exploitation of natural resources, including water, ores and hydrocarbons. * Completely revised edition; Like its precursor, it describes sediments from sand grains to sedimentary basins; Features up-to date account and critique of sequence and cyclostratigraphy * Extensively illustrated with photos and remotely sensed sea bed images describing sedimentary processes, products and depositional systems; Color plates illustrate sediment textures, lithologies, pore types, diagenetic textures, and carbonate and clastic sequence stratigraphic models* Emphasises the applications of sedimentology to the exploration for and exploitation of natural resources, including water, ores and hydrocarbons* Extensive references and up-to-date bibliography for further study
A good quality annual review series that provides an important service to the sciences for both the general and the specialist reader. Oceanography and Marine Biology has succeeded in producing one admirably for more than 35 years. The quality of the paper, the printing and the presentation is excellent.--Times Higher Education Supplement