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Titlebook: Deformation Microstructures in Rocks; Soumyajit Mukherjee Book 2013 Springer-Verlag Berlin Heidelberg 2013 Deformation.Microstructure.Micr

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發(fā)表于 2025-3-21 17:21:39 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Deformation Microstructures in Rocks
編輯Soumyajit Mukherjee
視頻videohttp://file.papertrans.cn/265/264828/264828.mp4
概述189 colour photos of microstructures.Many less known structures in micro-scale.Will act as a reference book for researchers and students.Includes supplementary material:
叢書名稱Springer Geochemistry/Mineralogy
圖書封面Titlebook: Deformation Microstructures in Rocks;  Soumyajit Mukherjee Book 2013 Springer-Verlag Berlin Heidelberg 2013 Deformation.Microstructure.Micr
描述Study of microstructures is an indispensable component of understanding structural geology of any terrain. A number of ‘new’ microscopic structures such as ‘flanking microstructures’, trapezoid-shaped mineral grains, reversal of ductile shear sense, micro-duplexes, V-pull aparts, and new minerals nucleating inside host minerals have recently been described in individual manuscripts. However, for the sake of brevity, microstructural papers cannot show all possible variation in their morphology. The proposed book aims to present these structures with attractive colour photographs. Each photomicrograph will have a comprehensive caption. The book also presents grain boundary migration, boudins, symptoms of metamorphic retrogression, and how well known shear sense indicators (S-C fabrics, mineral fish etc.) vary in morphology in serial-sections. The target audience is for graduate and postgraduate geosciences students and researchers of structural geology.
出版日期Book 2013
關(guān)鍵詞Deformation; Microstructure; Microtexture; Shear Zone; Structural Geology
版次1
doihttps://doi.org/10.1007/978-3-642-25608-0
isbn_softcover978-3-662-52141-0
isbn_ebook978-3-642-25608-0Series ISSN 2194-3176 Series E-ISSN 2194-3184
issn_series 2194-3176
copyrightSpringer-Verlag Berlin Heidelberg 2013
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 23:17:20 | 只看該作者
Book 2013ch as ‘flanking microstructures’, trapezoid-shaped mineral grains, reversal of ductile shear sense, micro-duplexes, V-pull aparts, and new minerals nucleating inside host minerals have recently been described in individual manuscripts. However, for the sake of brevity, microstructural papers cannot
板凳
發(fā)表于 2025-3-22 01:57:15 | 只看該作者
地板
發(fā)表于 2025-3-22 08:20:54 | 只看該作者
Springer Geochemistry/Mineralogyhttp://image.papertrans.cn/d/image/264828.jpg
5#
發(fā)表于 2025-3-22 10:54:26 | 只看該作者
https://doi.org/10.1007/978-3-642-25608-0Deformation; Microstructure; Microtexture; Shear Zone; Structural Geology
6#
發(fā)表于 2025-3-22 14:34:40 | 只看該作者
978-3-662-52141-0Springer-Verlag Berlin Heidelberg 2013
7#
發(fā)表于 2025-3-22 19:49:48 | 只看該作者
8#
發(fā)表于 2025-3-22 21:33:15 | 只看該作者
9#
發(fā)表于 2025-3-23 04:53:33 | 只看該作者
https://doi.org/10.1007/978-94-011-7888-4Passchier (2001) described ‘Flanking structures’ as ‘deflection of planar or linear fabric elements in a rock alongside a cross-cutting object’. Following this, a number of papers came up on its morphology and mechanism.
10#
發(fā)表于 2025-3-23 08:11:28 | 只看該作者
https://doi.org/10.1007/978-94-011-7888-4Intrafolial folds are tight to isoclinal syn-shear overturned folds in ductile shear zones. These folds could be bound by both primary–and secondary ductile shear planes.
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