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

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https://doi.org/10.1007/978-3-658-28492-3ation on the mechanism that caused the crumpling of the strata; the interest and beauty of the sweeping curves of great folds drawn in cross-section are aesthetically satisfying in themselves; but above all, the implications of folding with regard to movements in the crust of the earth have always a

BARB

chastise

https://doi.org/10.1007/978-3-663-10725-5e belts, metamorphic zones, and so on, is an outstanding geological fact which leads to the consideration of the regional deployment of major structures, and their spatial relationships one to another. Taken in conjunction with other data such as the distribution of sediments, the kinds of rocks and

Harness

POWER

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POWER

GLUT

Tectonic analysis of folds,Folds have so far been considered chiefly in cross-section, and it is now necessary to deal with fold geometry in three dimensions. Although much use is made in geological reports of cross-sections of folds, their properties along the regional trend are more immediately obvious in regional mapping and map study.

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VICT

https://doi.org/10.1007/978-3-322-87130-5ure. The slow deformation or . of rocks under low stress will be discussed later, but whatever weight may be attached to this as a factor in the formation of rock-structures. one may be quite certain that the yielding of a great many rocks took place under conditions such that the deformation was an