標(biāo)題: Titlebook: Deformation Processes in Minerals, Ceramics and Rocks; David J. Barber,Philip G. Meredith Book 1990 D. J. Barber, P. G. Meredith & contrib [打印本頁] 作者: 強(qiáng)烈興趣 時(shí)間: 2025-3-21 19:00
書目名稱Deformation Processes in Minerals, Ceramics and Rocks影響因子(影響力)
書目名稱Deformation Processes in Minerals, Ceramics and Rocks影響因子(影響力)學(xué)科排名
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書目名稱Deformation Processes in Minerals, Ceramics and Rocks網(wǎng)絡(luò)公開度學(xué)科排名
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書目名稱Deformation Processes in Minerals, Ceramics and Rocks讀者反饋
書目名稱Deformation Processes in Minerals, Ceramics and Rocks讀者反饋學(xué)科排名
作者: 外星人 時(shí)間: 2025-3-21 22:01 作者: BANAL 時(shí)間: 2025-3-22 02:17
Single-crack behaviour and crack statistics,f cracks, not necessarily isotropic and homogeneous, more or less interacting, so that the physical properties are those of a complex structure. In such a situation, understanding of the behaviour of a single crack may appear to be irrelevant. It should be looked at rather as a necessary, although n作者: Concomitant 時(shí)間: 2025-3-22 04:59
Fracture of polycrystalline ceramics, critical flaw dimensions increase in size from a scale less than characteristic micro-structure dimensions to a size which encompasses many grain diameters, the resistance to fracture increases, in certain polycrystals, by a factor of 5–10. This increase represents the difference between the fractu作者: 松馳 時(shí)間: 2025-3-22 12:04
Compressive brittle fracture and the construction of multi-axial failure maps,these cracks extend to the sample surface, or if they interact with each other so that they grow in an unstable manner, then a macroscopic failure may follow. The initiation and growth of cracks from pores has been considered by Sammis & Ashby (1986): that from small angled cracks is analysed by Nem作者: frenzy 時(shí)間: 2025-3-22 15:09
Brittle-to-ductile transitions in polycrystalline non-metallic materials,teristic strength and brittle or ductile deformation behaviour of crystalline solids is determined by the nature of their atomic bonding and crystal structure. Thus Frost & Ashby (1982) have recognized 21 isomechanical groups in their study of deformation mechanism maps to represent the plasticity a作者: frenzy 時(shí)間: 2025-3-22 18:17 作者: PLUMP 時(shí)間: 2025-3-23 00:35 作者: A簡潔的 時(shí)間: 2025-3-23 01:57 作者: 使人煩燥 時(shí)間: 2025-3-23 07:34 作者: 高腳酒杯 時(shí)間: 2025-3-23 11:21 作者: predict 時(shí)間: 2025-3-23 17:40 作者: iodides 時(shí)間: 2025-3-23 20:18
Densification of crystalline aggregates by fluid-phase diffusional creep,melt can deform by diffusive mass transfer through the grain-boundary liquid phase (Durney 1972, Robin 1978, Raj 1982, Rutter 1983, Cooper & Kohlstedt 1984). This type of mechanism is generally referred to as fluid-phase diffusional creep (Stocker & Ashby 1973), solution-precipitation creep (Raj 198作者: JUST 時(shí)間: 2025-3-23 22:32
Dynamic recrystallization and grain size,ory is attractive. While not attempting to be a review of palaeopiezometers, this chapter will present evidence for a ‘universal relation’ between deformation stress and the steady-state recrystallized grain size resulting from stress-induced boundary migration. This law is, of course, derived from 作者: 秘密會(huì)議 時(shí)間: 2025-3-24 05:02
Simulation of dislocation-assisted plastic deformation in olivine polycrystals,4, Christensen 1987), which is believed to be the major constituent of the upper mantle. The mantle is assumed to deform in a régime of steady-state creep in which diffusion and dislocation glide occur. When dislocation glide is present, polycrystalline materials develop anisotropy due to rotations 作者: Amorous 時(shí)間: 2025-3-24 09:30 作者: Curmudgeon 時(shí)間: 2025-3-24 11:34
A TEM study of dislocation reactions in experimentally deformed chalcopyrite single crystals,ure conditions in the shallow Earth’s crust. The understanding of the mechanical behaviour of the common sulphide ore minerals, galena, sphalerite, pyrite, pyrrhotite, and chalcopyrite, has progressed on account of numerous deformation studies in the laboratory over a variety of experimental conditi作者: 隱士 時(shí)間: 2025-3-24 16:26
https://doi.org/10.1007/978-3-319-21335-4r in the Preface. The additional contributions were judged to be needed in order to make the monograph more comprehensive and self-sufficient. In particular, there are two overviews written by the individual editors, which are intended to give the necessary frameworks and references to relevant prev作者: MAG 時(shí)間: 2025-3-24 21:50 作者: A保存的 時(shí)間: 2025-3-25 00:51 作者: Surgeon 時(shí)間: 2025-3-25 07:05 作者: Asymptomatic 時(shí)間: 2025-3-25 08:28
Jozef Rovensky,Juraj Payer,Manfred Heroldthese cracks extend to the sample surface, or if they interact with each other so that they grow in an unstable manner, then a macroscopic failure may follow. The initiation and growth of cracks from pores has been considered by Sammis & Ashby (1986): that from small angled cracks is analysed by Nem作者: exhilaration 時(shí)間: 2025-3-25 14:34 作者: APNEA 時(shí)間: 2025-3-25 18:37 作者: hyperuricemia 時(shí)間: 2025-3-25 22:47 作者: Infirm 時(shí)間: 2025-3-26 01:58
https://doi.org/10.1007/978-94-011-2294-8macroscale structures in naturally deformed rocks, in terms of the . and . conditions of deformation, the flow stresses and finite strains, and whether the deformation was brittle or ductile, seismic or aseismic. Second they provide data which can be used in . modelling of the thermomechanical evolu作者: 一夫一妻制 時(shí)間: 2025-3-26 06:54
https://doi.org/10.1007/978-94-011-2294-8 mechanisms, rates and conditions during tectonic events (Borradaile .. 1982, Schmid 1982, Hobbs & Heard 1986, Tullis 1986, Wang 1986, Atkinson 1987, Schmid .. 1987, Knipe & Rutter 1990). The microstructures characteristic of different deformation mechanisms, which operate under different deformatio作者: anthesis 時(shí)間: 2025-3-26 08:41 作者: 食料 時(shí)間: 2025-3-26 14:14
https://doi.org/10.1007/978-94-011-2294-8ses in which ‘mechanical force is resolved into chemical action’. Sorby later coined the term ‘pressure solution’ in ascribing phenomena such as the pitting of pebbles (Mosher 1981) to stress-enhanced solubility, with which he was familiar from contemporary work in physical chemistry (Durney 1978). 作者: 沙漠 時(shí)間: 2025-3-26 17:21 作者: 使人煩燥 時(shí)間: 2025-3-26 23:56
https://doi.org/10.1007/978-94-011-2294-8ory is attractive. While not attempting to be a review of palaeopiezometers, this chapter will present evidence for a ‘universal relation’ between deformation stress and the steady-state recrystallized grain size resulting from stress-induced boundary migration. This law is, of course, derived from 作者: 擴(kuò)大 時(shí)間: 2025-3-27 05:04
https://doi.org/10.1007/978-94-011-2294-84, Christensen 1987), which is believed to be the major constituent of the upper mantle. The mantle is assumed to deform in a régime of steady-state creep in which diffusion and dislocation glide occur. When dislocation glide is present, polycrystalline materials develop anisotropy due to rotations 作者: 減至最低 時(shí)間: 2025-3-27 05:39
https://doi.org/10.1007/978-94-011-2294-8 various physical properties with the O: U ratio has considerable technological significance, as use of UO. based nuclear fuels necessarily encompasses a large region of the .-. space of Fig. 15.1. Plastic deformation in UO. has been of interest since the earliest uses of UO. as a nuclear fuel, sinc作者: Counteract 時(shí)間: 2025-3-27 10:17
https://doi.org/10.1007/978-94-011-2294-8ure conditions in the shallow Earth’s crust. The understanding of the mechanical behaviour of the common sulphide ore minerals, galena, sphalerite, pyrite, pyrrhotite, and chalcopyrite, has progressed on account of numerous deformation studies in the laboratory over a variety of experimental conditi作者: 表示問 時(shí)間: 2025-3-27 14:15
The Mineralogical Society Serieshttp://image.papertrans.cn/d/image/264830.jpg作者: 修飾 時(shí)間: 2025-3-27 20:08
https://doi.org/10.1007/978-94-011-2294-8 been transferred almost in totality from the practice of physical metallurgy. Indeed, even in the newer field of materials science, dealing with ceramics and other materials, the traditional methods for deriving rheological laws from high-temperature creep experiments have been religiously handed down from adviser to student.作者: 男學(xué)院 時(shí)間: 2025-3-28 01:33
https://doi.org/10.1007/978-94-011-6827-4ceramics; formation; mineral; mineral resources作者: minion 時(shí)間: 2025-3-28 04:42
978-94-011-6829-8D. J. Barber, P. G. Meredith & contributors 1990作者: monologue 時(shí)間: 2025-3-28 10:18
Experimental deformation and data processing, been transferred almost in totality from the practice of physical metallurgy. Indeed, even in the newer field of materials science, dealing with ceramics and other materials, the traditional methods for deriving rheological laws from high-temperature creep experiments have been religiously handed down from adviser to student.作者: Annotate 時(shí)間: 2025-3-28 12:13 作者: padding 時(shí)間: 2025-3-28 16:42 作者: 攀登 時(shí)間: 2025-3-28 21:09
Jozef Rovensky,Juraj Payer,Manfred Herold to engineering structures or to mechanics of the Earth’s crust). This arises in part from an emphasis on phenomenological aspects of macroscopic deformation and failure at the expense of micromechanical aspects of fracture, and in part from the rate, size, and environment dependence of the brittle 作者: contrast-medium 時(shí)間: 2025-3-28 22:54
Jozef Rovensky,Juraj Payer,Manfred Heroldopic level (Lawn & Wilshaw 1975, Section 3.3). Macroscopic behaviour is to be interpreted in terms of microscopic processes. As far as cracks are concerned, important microscopic processes are nucleation and propagation of extensional cracks. However, in order to take into account the fact that a re作者: voluble 時(shí)間: 2025-3-29 07:00 作者: 樣式 時(shí)間: 2025-3-29 08:31
Jozef Rovensky,Juraj Payer,Manfred Heroldee are the three classes of metals with cubic crystal structures — f.c.c., b.c.c, and h.c.p.), showing a progression of plastic flow properties (Frost & Ashby 1982, Tables 18.3 & 18.4) and of cleavage properties (Kelly, Tyson & Cottrell 1967; Gandhi & Ashby 1979, Table 4 & Fig. 28). These are illust作者: POINT 時(shí)間: 2025-3-29 13:59 作者: GONG 時(shí)間: 2025-3-29 18:21
https://doi.org/10.1007/978-94-011-2294-8aws are adequate to describe the diffusion-controlled plastic deformation (e.g. Karato .. 1986), they do not take account of plastic anisotropy due to slip. We attempt to introduce a generalized description of anisotropic plastic flow of olivine based on polycrystal plasticity theory which takes int作者: grenade 時(shí)間: 2025-3-29 20:48 作者: 完成才會(huì)征服 時(shí)間: 2025-3-30 03:22
https://doi.org/10.1007/978-94-011-2294-8n deformed marcasite (Fagot .. 1981), and has provided detailed information on the ductile behaviour of pyrite (Cox .. 1981, Graf .. 1981, Levade .. 1982) and sphalerite (Levade .. 1986). Previous interpretations of the flow mechanisms in experimentally deformed polycrystalline chalcopyrite resulted作者: 使苦惱 時(shí)間: 2025-3-30 05:14
Deformation Processes in Minerals, Ceramics and Rocks作者: 聲音刺耳 時(shí)間: 2025-3-30 11:15
Deformation Processes in Minerals, Ceramics and Rocks978-94-011-6827-4作者: BOLUS 時(shí)間: 2025-3-30 13:41 作者: Decline 時(shí)間: 2025-3-30 18:06 作者: 哺乳動(dòng)物 時(shí)間: 2025-3-31 00:23 作者: ensemble 時(shí)間: 2025-3-31 04:31
Brittle-to-ductile transitions in polycrystalline non-metallic materials,ee are the three classes of metals with cubic crystal structures — f.c.c., b.c.c, and h.c.p.), showing a progression of plastic flow properties (Frost & Ashby 1982, Tables 18.3 & 18.4) and of cleavage properties (Kelly, Tyson & Cottrell 1967; Gandhi & Ashby 1979, Table 4 & Fig. 28). These are illust作者: GRATE 時(shí)間: 2025-3-31 05:25
,Régimes of plastic deformation — processes and microstructures: an overview,tion between the two opposed behaviours under experimental conditions are well known (see, for example, Hobbs .., 1976, p. 62). Factors bearing on the transition have already been discussed in the chapter by Murrell (this volume).作者: 膽大 時(shí)間: 2025-3-31 12:43 作者: recession 時(shí)間: 2025-3-31 14:10
