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Titlebook: Structural Geology; A.R. Bhattacharya Book 2022 Springer Nature Switzerland AG 2022 Structural geology.Rock deformation.Geometry and genes

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Foliation deformation and is uniformly pervasive in a rock. Foliation is commonly developed in metamorphic rocks and includes cleavage, schistosity, gneissosity and gneissic banding. . or . is a planar fabric along which rocks easily split or cleave into parallel or subparallel surfaces formed during metamor
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Lineationeveloped on the surface of rocks, it may also penetrate to a small extent, up to a few millimetres only. As such, lineation is broadly grouped as . such as slickensides, slickenlines and slickenfibres and . such as mineral lineation, crenulation lineation, intersection lineation, boudins, mullions,
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Mechanisms of Rock Deformationl past. A . broadly means the process that tends to accommodate large strains in rocks, thus leading to a stable structure/microstructure to the rock. The processes operate on different scales, but those operating on grain scales bring about significant changes to the structure and texture of rocks.
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Concept of Deformationt of stress is sometimes visible and sometimes not, depending upon the strength of a rock with respect to the applied stress..This chapter takes the readers to explore the concept of deformation of rocks with the necessary elementary ideas so that their journey to structural geology may not become an uphill task!
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2510-1307 n each chapter expand the horizons of the reader on the subject matter of the chapter. Questions at the end of each chapter, and detailed significance of the key structures, provide a better grasping to student978-3-030-80797-9978-3-030-80795-5Series ISSN 2510-1307 Series E-ISSN 2510-1315
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w problem is a natural generalization of the distinguishability problem between two probability distributions, which are commonly used in computational cryptography. We show that the problem has several cryptographic properties and they enable us to construct a quantum publickey cryptosystem, which
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