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Titlebook: Microtectonics; Cees W. Passchier,R. A. J. Trouw Textbook 2005Latest edition Springer-Verlag Berlin Heidelberg 2005 Deformation.Microtecto

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11#
發(fā)表于 2025-3-23 12:35:31 | 只看該作者
rphotoreceptor matrix in the subretinal space. Two important receptor-mediated interactions between the apical surface of the retinal pigment epithelium (RPE) and adjacent photoreceptors are adhesion ensuring outer segment alignment and diurnal phagocytosis of shed outer segment fragments contributi
12#
發(fā)表于 2025-3-23 17:23:58 | 只看該作者
13#
發(fā)表于 2025-3-23 21:22:04 | 只看該作者
A Framework of Microtectonic Studies,raphic, has evolved during the last century to include a number of structural characteristics, that constitute the microstructure or fabric of a rock. The study of this fabric can be used to reconstruct the structural and metamorphic history, but also to improve the understanding of deformation and
14#
發(fā)表于 2025-3-23 23:17:44 | 只看該作者
Flow and Deformation,ng simple concepts and illustrations. Continuum mechanics is a subject that is considered to be difficult by many students, and seen as too theoretical to be of practical use in the interpretation of geological structures. It is true that it is rarely possible to make detailed reconstructions of flo
15#
發(fā)表于 2025-3-24 04:05:11 | 只看該作者
Deformation Mechanisms, crust or at high strain rate. At deeper crustal levels, rocks deform by ductile flow through a range of mechanisms of ductile grain scale deformation such as dissolutionprecipitation, intracrystalline deformation by dislocation glide and creep, diffusion creep, twinning and kinking. Ductile deforma
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發(fā)表于 2025-3-24 07:20:40 | 只看該作者
17#
發(fā)表于 2025-3-24 10:53:51 | 只看該作者
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發(fā)表于 2025-3-24 18:51:39 | 只看該作者
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發(fā)表于 2025-3-24 21:34:44 | 只看該作者
20#
發(fā)表于 2025-3-25 00:23:09 | 只看該作者
Primary Structures,es from metamorphic rocks. This problem may appear in low grade metasediments and in igneous rocks that were subjected to solid state deformation after crystallisation..In igneous rocks and in migmatites a distinction can be made between magmatic, submagmatic and solid state flow. Criteria to recogn
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