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

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发表于 2025-3-21 18:08:16 | 显示全部楼层 |阅读模式
书目名称Introduction to Small~scale Geological Structures
编辑Gilbert Wilson
视频video
图书封面Titlebook: Introduction to Small~scale Geological Structures;  Gilbert Wilson Book 1982 G. Wilson 1982 formation.fossil.fracture.history.stratigraphy.
描述The small-scale structures referred to in this publication are those structures of tectonic origin that can be observed with the naked eye in 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 unknown origin. Recognition of these minor structures, and appreciation of their origin and significance assist the field geologist to elucidate the larger-scale geological structures of his area. Commonly some can be used in deciphering the order of strati­ graphic succession in regions of strongly-folded unfossiliferous beds; and, in ground which has suffered superposed tectonic movements, the minor structures may provide evidence of successive phases or events in the tectonic history. The work contains descriptions of the more common varieties of small-scale tectonic structures, the different ways in which these structures may have been formed, and the limitations of the conclusions which can be drawn from their observation in the field. Gilbert Wils
出版日期Book 1982
关键词formation; fossil; fracture; history; stratigraphy; symmetry; tectonics
版次1
doihttps://doi.org/10.1007/978-94-011-6838-0
isbn_softcover978-94-011-6840-3
isbn_ebook978-94-011-6838-0
copyrightG. Wilson 1982
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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.
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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.
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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).
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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
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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
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