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Applied Sedimentology, Second Edition by Richard C. Selley

By Richard C. Selley

There are 3 varieties 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 strategies that modify gentle sediment into sedimentary rock. Sedimentary rocks contain sandstones, limestones and mudstones. all of the world's coal, so much of its water and fossil fuels, and plenty of mineral deposits happen in sedimentary rocks. utilized Sedimentology exhibits how the learn of sediments aids the exploration for and exploitation of common assets, together with water, ores and hydrocarbons. * thoroughly revised version; Like its precursor, it describes sediments from sand grains to sedimentary basins; positive aspects up-to date account and critique of series and cyclostratigraphy * commonly illustrated with pictures and remotely sensed sea mattress photographs describing sedimentary strategies, items and depositional platforms; colour plates illustrate sediment textures, lithologies, pore forms, diagenetic textures, and carbonate and clastic series stratigraphic types* Emphasises the purposes of sedimentology to the exploration for and exploitation of traditional assets, together with water, ores and hydrocarbons* large references and updated bibliography for additional learn

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The residua are the insoluble products of weathering, which range in size from boulders down to colloidal clay particles. 2 THE SEDIMENTARYCYCLE 23 Fig. 1. The Rocks Display'd (from Wilson, in Read, 1944),illustrating that the sedimentary cycle is a small part of the whole crustal cycle of the dynamicearth. Individual sedimentary grains of stable minerals, principally quartz, may be recycled several times before being destroyed by metamorphism. Courtesyof the Geologists' Association. handle and segregate the products of weathering.

The folklore of geology records that windblown sand grains have opaque frosted surfaces, while water-laid sands have clear translucent surfaces. Kuenen and Perdok (1962) attributed frosting not to the abrasive action of wind and water but to alternate solution and precipitation under subaerial conditions. Electron microscopic studies show that there are several types of surface texture on sand grains produced by glacial, eolian, and aqueous processes (Krinsley, 1998). The 41 42 3 PARTICLES, PORES, AND PERMEABILITY surfaces of water-deposited sand grains are characterized by V-shaped percussion pits and grooves.

275-288. REFERENCES 39 Buchanan, E (1807). "A Journey from Madras Through the Counties of Mysore, Kanara and Malabar," 3 vols. East India Company, London. Chapman, R. W. (1974). Calcareous duricrust in A1-Hasa, Saudi Arabia. Geol. Soc. Am. Bull. 85, 119-130. Cox, D. , and Singer, D. A. (1986). Mineral deposit models. Geol. Surv. Bull. ) 1693,1-379. Curtis, C. D. (1976). Stability of minerals in surface weathering reactions. Earth Surf. Processes 1, 63-70. Edwards, R. A. (1976). Tertiary sediments and structure of the Bovey Tracey basin, South Devon.

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