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Fold terminology (R.P. - 8.3.2.1, 8.3.2.3)Date: 2015-10-07; view: 538. WORD FORMATION
VERBS (+ PREPOSITION) to drape over – ниспадать складками; to precede – предшествовать; to manifest – проявляться, становиться явным; adjacent to – смежный, расположенный рядом; to converge upon – стремиться к пределу; to associate with – связывать с, ассоциировать с. Folding in layered rocks consists of deformation of strata without faulting. Folds are formed by compression, draping over basement blocks, and compaction. Faulting often accompanies folding and can precede it or follow it. The triaxial stress system for folding is representative for faulting since the two are intimately related. Folds are manifested as different types according to morphology, origin and type of internal deformation. General fold terminology is descriptive and relates to elements of individual features applicable to all types of folds 1. Anticline is a fold with upward convexity. Beds that make up an anticline dip in opposite directions away from the crest or high point of the fold. 2. Syncline is a concave upward. Beds making up a syncline dip in opposite directions toward the trough, or low point of the fold.
7. A fold is symmetrical when its shape and mirror image are identical or when the fold is bilaterally symmetrical about the hinge surface. Symmetrical folds are usually represented by a vertical hinge surface. 8. A fold that is not bilaterally symmetrical about the hinge surface is asymmetrical. Its hinge surface is usually inclined. (Абрамова Р.Н., Квеско Н.Г., Introduction to Continuum Mechanics- учебное пособие, Томск, ТПУ. 2005.)
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