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Applied Sedimentology, Second Edition - download pdf or read online

By Richard C. Selley

ISBN-10: 0080527477

ISBN-13: 9780080527475

ISBN-10: 0126363757

ISBN-13: 9780126363753

There are 3 different types of rock-igneous, metamorphic and sedimentary. Sedimentary rocks shape from the weathering, erosion, transportation and deposition of older rocks. utilized Sedimentology describes the formation, transportation and deposition of sediment, and the post-depositional procedures that modify delicate sediment into sedimentary rock. Sedimentary rocks comprise sandstones, limestones and mudstones. the entire world's coal, such a lot of its water and fossil fuels, and lots of mineral deposits ensue in sedimentary rocks. utilized Sedimentology indicates how the research of sediments aids the exploration for and exploitation of usual assets, together with water, ores and hydrocarbons. * thoroughly revised variation; Like its precursor, it describes sediments from sand grains to sedimentary basins; beneficial properties up-to date account and critique of series and cyclostratigraphy * generally illustrated with pictures and remotely sensed sea mattress pictures describing sedimentary approaches, items and depositional platforms; colour plates illustrate sediment textures, lithologies, pore varieties, diagenetic textures, and carbonate and clastic series stratigraphic versions* Emphasises the purposes of sedimentology to the exploration for and exploitation of typical assets, together with water, ores and hydrocarbons* huge references and updated bibliography for extra examine

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Additional resources for Applied Sedimentology, Second Edition

Example text

4). Friedman (1958, 1962) has empirically derived methods for converting grain size data from thin sections to sieve analyses. 1 PHYSICAL PROPERTIES OF PARTICLES 47 Plane of thin section Fig. 4. Sketch showing how grain size determined by measuring grain diameters from thin sections will always give too low an average reading, because particles will normally be dissected at less than their true diameters. This problem can be overcome by using the statistical gymnastics described in the text. 2).

6). The rocks immediately beneath an unconformity are often intensely weathered, but Fig. 6. Cross-sections through fossil soil (paleosol) horizons. (Left) Coal bed (black) with seat earth beneath. This is a white, bleached, kaolinitic sandstone pierced by plant roots. Based on examples in the Coal Measures (Carboniferous) of England. (Right) Caliche soil horizon of nodular carbonate in red fluvial siltstone. Reworked caliche pebbles in the overlying channel sand testify to penecontemporaneous formation.

1998). Late Dinantian palaeokarst of England and Wales: Implications for exposure surface development. Sedimentology 45, 19-38. Webber, B. N. (1972). Supergene nickel deposits. Trans. Soc. Pet. Eng. A I M E 252, 333-347. Williams, G. E. (1969). Characteristics and origin of a PreCambrian pediment. J. Geol. 77, 183207. Williams, J. J. (1968). The stratigraphy and igneous reservoirs of the Augila field, Libya. In "Geology and Archaeology of Northern Cyrenaica, Libya" (F. T. ), pp. 197-207. Pet. Explor.

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Applied Sedimentology, Second Edition by Richard C. Selley


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