Titlebook: Introduction to Small~scale Geological Structures; Gilbert Wilson Book 1982 G. Wilson 1982 formation.fossil.fracture.history.stratigraphy.

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Harrowing

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神刊

鳥籠

Antagonism

Minor structures and large-scale tectonics,s in tectonic style, rates of movement, and the relative ages of impulses during the evolution of the major structure will all influence the types of structures that may be produced and their relationships to each other.

brassy

Introduction,ical studies — are commonly presented to the reader in a form which frightens the non-specialist to such an extent that he either leaves the subject entirely alone, or he loses himself in a maze of detail and jargon.

邊緣

Flow cleavage, schistosity and lineation,r stretching in the production of slaty cleavage; but in many textbooks this factor is ignored, and reference is only made to the fact that the rocks have been subjected to pressure. The importance of, and the evidence for such stretching have been summarised by Fourmarier (1949b).

異常

n the field. Their scale varies broadly between that of the hand-specimen to that of the exposure, or even mountainside. Such structures are the visible effects of rock deformation caused by local stresses and movements which have been induced in the rocks by external tectonic forces of possibly unk

機(jī)構(gòu)

Book 1982d. Their scale varies broadly between that of the hand-specimen to that of the exposure, or even mountainside. Such structures are the visible effects of rock deformation caused by local stresses and movements which have been induced in the rocks by external tectonic forces of possibly unknown origi