EVOKE
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发表于 2025-3-21 23:03:34
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Harrowing
发表于 2025-3-22 00:31:51
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神刊
发表于 2025-3-22 05:35:31
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鸟笼
发表于 2025-3-22 11:54:32
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Antagonism
发表于 2025-3-22 13:01:23
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
发表于 2025-3-22 17:13:02
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.
边缘
发表于 2025-3-22 22:15:39
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).
异常
发表于 2025-3-23 02:48:59
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
机构
发表于 2025-3-23 08:28:58
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