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Titlebook: Evolution of Geological Structures in Micro- to Macro-scales; S. Sengupta Book 1997 Springer Science+Business Media Dordrecht 1997 Deforma

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书目名称Evolution of Geological Structures in Micro- to Macro-scales
编辑S. Sengupta
视频video
图书封面Titlebook: Evolution of Geological Structures in Micro- to Macro-scales;  S. Sengupta Book 1997 Springer Science+Business Media Dordrecht 1997 Deforma
描述Structural geology has developed at a very rapid pace inrecent years. .Evolution of Geological Structures in Micro- toMacro-Scales., covering a wide spectrum of current research instructural geology from the grain scale to the scale of orogenic beltsand from the brittle to the ductile field, provides an overview ofnewly emerging concepts in a single volume. The book covers a widerange of advances in such broad fields as hydraulic factures, normalfaults, overthrusts, ductile shear zones, rock fabrics, folds,superposed folds and basement structures.
出版日期Book 1997
关键词Deformation; Dyke; crystallography; fault; orogenic belt; orogeny; structural geology
版次1
doihttps://doi.org/10.1007/978-94-011-5870-1
isbn_softcover978-94-010-6481-1
isbn_ebook978-94-011-5870-1
copyrightSpringer Science+Business Media Dordrecht 1997
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Overthrust shear in mountain buildingformation is needed. This is the result of an analysis of a comprehensive data set, comprising fold axial plane and cleavage orientations, and finite and incremental strain. There is a tendency for the strain to be concentrated at the nappe boundaries. The orientation of the finite strain stretching
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Practical analysis of general shear zones using the porphyroclast hyperbolic distribution method: An76), among others. In general shear zones, rigid ellipsoidal grains may rotate either forwards (with the sense of shear) or backwards (counter to the sense of shear) according to their axial ratios and orientations. Grains of a critical shape have their forward motion exactly countered by backward m
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