Titlebook: Deformation Processes in Minerals, Ceramics and Rocks; David J. Barber,Philip G. Meredith Book 1990 D. J. Barber, P. G. Meredith & contrib

高腳酒杯

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iodides

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

JUST

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

秘密會議

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

Amorous

Curmudgeon

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

隱士

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

MAG

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