Titlebook: Elements of Structural Geology; E. Sherbon Hills Book 1972 E. Sherbon Hills 1972 fault.structural geology.tectonics

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Overview: 978-0-412-20750-1978-94-009-5843-2

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Managing with Sense and Sensitivityn of rock-structures. Without for the moment defining precisely what is meant by rock-structures, let us consider any geological cross-section showing beds in various attitudes — flat-lying or inclined, folded or faulted — perhaps in places intruded by igneous rocks or covered with lava-flows, and a

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Managing your Mental Health during your PhData in a sedimentary succession, and the presence within any one bed of a fine lamination or texture which is connected with its deposition (Fig. II-1). In general each bed is fairly homogeneous and may be distinguished from other beds by some characteristic feature such as texture (e.g. shale, sand

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https://doi.org/10.1007/978-981-10-1035-4es, including both those which being visible to the naked eye may be mapped in the field, and those that can be determined only under the microscope, and must accordingly be studied in the laboratory. In this chapter we shall deal with macro-structures, and later (Chapter XIII) with structural petro

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https://doi.org/10.1007/978-3-322-93235-8lt refers both to the plane itself, which is called the ., and to the displacements that have gone on along it. In conformity with the ideas on plastic slip and shear-fracturing expressed in Chapter III, fault planes may be shear-fractures along which the internal cohesion of the rocks has been dest