標題: Titlebook: Atlas of Mylonites - and related microstructures; Rudolph A. J. Trouw,Cees W. Passchier,Dirk J. Wier Book 2010 Springer-Verlag Berlin Heid [打印本頁] 作者: Inoculare 時間: 2025-3-21 19:01
書目名稱Atlas of Mylonites - and related microstructures影響因子(影響力)
書目名稱Atlas of Mylonites - and related microstructures影響因子(影響力)學科排名
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書目名稱Atlas of Mylonites - and related microstructures網(wǎng)絡公開度學科排名
書目名稱Atlas of Mylonites - and related microstructures被引頻次
書目名稱Atlas of Mylonites - and related microstructures被引頻次學科排名
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書目名稱Atlas of Mylonites - and related microstructures年度引用學科排名
書目名稱Atlas of Mylonites - and related microstructures讀者反饋
書目名稱Atlas of Mylonites - and related microstructures讀者反饋學科排名
作者: ambivalence 時間: 2025-3-21 23:36 作者: SEVER 時間: 2025-3-22 01:12 作者: 焦慮 時間: 2025-3-22 07:45 作者: Incorporate 時間: 2025-3-22 12:29 作者: maintenance 時間: 2025-3-22 14:09
Further Applications to Lie Algebrasform the matrix rather then the porphyroclasts. An exeption to this are mylonitised ignimbrites or other volcanic rocks (e.g. Figs. 9.5.46 and 9.5.47; Passchier & Trouw 2005, their Figs. 3.9 and 3.10).作者: 奴才 時間: 2025-3-22 19:01
Book 2010the metamorphic circumstances during mylonitization? What was the intensity of deformation?, and What was the sense of shear?..This book will complement the very successful textbook "Microtectonics" by Passchier and Trouw..作者: SEVER 時間: 2025-3-22 22:39
es and the contexts within which they formed.Includes supple.Mylonites form in response to high rates of strain within deep ductile shear zones, which are the extensions at depth of surface faults, thrusts and fault breccias, They can have many different mineralogical compositions and are therefore 作者: stratum-corneum 時間: 2025-3-23 03:26
The Strong Degree and the FI-Degreeystal-plastic processes as shown by its change in shape and by undulose extinction. At increasing temperature bulging recrystallisation starts to manifest itself along the lobate contacts and eventually recrystallisation by subgrain rotation takes over (Chapter 10).作者: 大炮 時間: 2025-3-23 07:40
The Strong Degree and the FI-Degreeand (forming porphyroclasts). Another group of rocks that readily forms mylonites are impure quartzites in which resistant minerals tend to form fish-like structures, again, by strong contrast in rheological behaviour.作者: Measured 時間: 2025-3-23 10:57 作者: 枯燥 時間: 2025-3-23 17:10 作者: 針葉 時間: 2025-3-23 20:46 作者: 寬宏大量 時間: 2025-3-24 00:41 作者: 含沙射影 時間: 2025-3-24 06:25
,“False” mylonites,form the matrix rather then the porphyroclasts. An exeption to this are mylonitised ignimbrites or other volcanic rocks (e.g. Figs. 9.5.46 and 9.5.47; Passchier & Trouw 2005, their Figs. 3.9 and 3.10).作者: 滔滔不絕地講 時間: 2025-3-24 08:44 作者: Pert敏捷 時間: 2025-3-24 12:59 作者: 連鎖 時間: 2025-3-24 17:53
Functional Hydrogels as Biomaterialsrained or glassy matrix with inclusions of wall-rock fragments. Commonly, a straight main fault vein (Sibson 1975; Spray 1992) representing a generation surface (Fig. 1.1) is present, from which smaller injection veins branch out. The main criteria to distinguish pseudotachylytes from cataclasites a作者: 過份艷麗 時間: 2025-3-24 21:28 作者: BILK 時間: 2025-3-24 23:56 作者: 琺瑯 時間: 2025-3-25 07:10 作者: Antagonist 時間: 2025-3-25 08:12
The Strong Degree and the FI-Degreeion of mylonites because of the contrasting behaviour of quartz and biotite on the one hand (forming matrix) and feldspar and muscovite on the other hand (forming porphyroclasts). Another group of rocks that readily forms mylonites are impure quartzites in which resistant minerals tend to form fish-作者: 古文字學 時間: 2025-3-25 12:52 作者: 攝取 時間: 2025-3-25 16:33 作者: 繁榮地區(qū) 時間: 2025-3-25 21:06
The Strong Degree and the FI-DegreeThe temperature range for the formation of this group of mylonites is approximately 500 to 650 °C. In medium-grade mylonites quartz is usually fully recrystallised, mainly by subgrain rotation, and has grown to a polygonal crystalloblastic fabric of strain free grains with an average grain size exceeding about 50 micrometers.作者: photophobia 時間: 2025-3-26 01:17 作者: apropos 時間: 2025-3-26 05:33
Functional Identities in (Semi)prime RingsThe purpose of this chapter is to give the reader the option to check his or her level of understanding of mylonites by trying to answer the questions given in the figure captions. Although we do not claim that our solutions given at the end of the chapter are the only possible ones, they will enable an assessment of the level of comprehension.作者: CURT 時間: 2025-3-26 10:55 作者: 摻和 時間: 2025-3-26 13:31 作者: MAG 時間: 2025-3-26 20:39 作者: limber 時間: 2025-3-26 22:20 作者: 縫紉 時間: 2025-3-27 05:00 作者: conservative 時間: 2025-3-27 05:49 作者: 躺下殘殺 時間: 2025-3-27 09:47 作者: 同位素 時間: 2025-3-27 17:29 作者: Simulate 時間: 2025-3-27 18:29
https://doi.org/10.1007/978-3-642-03608-8Cataclasite; Deformation; Mylonite; Pseudotachylyte; Shear sense indicators; Shear zone作者: 蛤肉 時間: 2025-3-27 23:22
978-3-662-50192-4Springer-Verlag Berlin Heidelberg 2010作者: gastritis 時間: 2025-3-28 03:05 作者: linguistics 時間: 2025-3-28 09:27
Functional Hydrogels as Biomaterialsrained or glassy matrix with inclusions of wall-rock fragments. Commonly, a straight main fault vein (Sibson 1975; Spray 1992) representing a generation surface (Fig. 1.1) is present, from which smaller injection veins branch out. The main criteria to distinguish pseudotachylytes from cataclasites are作者: 敲詐 時間: 2025-3-28 11:58 作者: LATER 時間: 2025-3-28 16:48
Introduction,ks (e.g. Shelley 1993; Snoke et al. 1998; Blenkinsop 2000; Vernon 2004; Passchier & Trouw 2005) and in many articles referred to in these books. Especially the excellent photographic atlas by Snoke et al. (1998) gives an extensive overview of current ideas on nomenclature and processes related to fa作者: nuclear-tests 時間: 2025-3-28 22:36 作者: seduce 時間: 2025-3-28 23:15 作者: Binge-Drinking 時間: 2025-3-29 05:41
Low-Grade Mylonites,grade mylonites. Whereas many feldspar porphyroclasts in low-grade mylonites still show fracturing by cataclasis, the quartz is usually deformed by crystal-plastic processes as shown by its change in shape and by undulose extinction. At increasing temperature bulging recrystallisation starts to mani作者: 星球的光亮度 時間: 2025-3-29 10:37 作者: CHANT 時間: 2025-3-29 12:36
Protomylonite, Mylonite and Ultramylonite,bserved in low-grade mylonites where the percentage of porphyroclasts decreases progressively with strain intensity. However, the percentage of matrix is highly dependent on mineralogical composition (e.g. quartz and biotite tend to convert to matrix readily). Compositional banding in gneiss can the作者: WATER 時間: 2025-3-29 16:29 作者: 代理人 時間: 2025-3-29 22:18 作者: 灌輸 時間: 2025-3-30 02:27
,“False” mylonites,is section. Low grade metasedimentary wackes containing detrital quartz grains in a fine-grained matrix may resemble mylonites. The quartz may show undulose extinction and resemble porphyroclasts in a mylonite (compare Fig. 10.2). However, in real mylonites quartz is the weaker mineral and tends to 作者: Culmination 時間: 2025-3-30 06:04
from what type of rock did this mylonite derive? What were the metamorphic circumstances during mylonitization? What was the intensity of deformation?, and What was the sense of shear?..This book will complement the very successful textbook "Microtectonics" by Passchier and Trouw..978-3-662-50192-4978-3-642-03608-8作者: Hyaluronic-Acid 時間: 2025-3-30 08:31
