纤细
发表于 2025-3-26 23:07:59
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打谷工具
发表于 2025-3-27 03:53:42
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爱哭
发表于 2025-3-27 07:16:41
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CROAK
发表于 2025-3-27 10:40:13
The Influence of Defect Crystallography on Some Properties of Orthosilicates,sch, 1982). Despite this recent interest in dislocation mechanisms, a notable limitation of many of these applications is the lack of a realistic concept of the structure of a mineral dislocation and how the crystallography of mineral defects affects their transport, interaction, and chemical properties.
轻信
发表于 2025-3-27 16:06:17
Kinetics of Metamorphic Reactions at Elevated Temperatures and Pressures: An Appraisal of Availables well as thermodynamically incompatible phases, irregular grain boundaries, and oriented fabrics. A great variety of environmental factors (presence of fluid, deformation, local chemical catalysts, etc.) can influence the kinetics of most mineral transformations. However, it is not often possible t
不可思议
发表于 2025-3-27 20:26:03
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DOLT
发表于 2025-3-28 00:47:36
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考博
发表于 2025-3-28 04:17:42
Heterogeneous Deformation, Foliation Development, and Metamorphic Processes in a Polyphase Mylonitems and strain paths from crystallographic fabrics, together with estimating stress levels from microstructural features (White .., 1980; Weathers .., 1979; Garcia Celma, 1982; Lister and Price, 1978; Law .., 1984).
gene-therapy
发表于 2025-3-28 08:50:12
Aspects of Relationships between Deformation and Prograde Metamorphism that Causes Evolution of WatMurrell, 1958) to show that the effective compressive stresses in the rock were reduced (and the effective tensile stresses increased) by an amount equal to the pore pressure, and that this was in good agreement with the available experimental data (Murrell, 1963, 1965). This was later extended to a
窃喜
发表于 2025-3-28 11:55:53
The Possible Effects of Deformation on Chemical Processes in Metamorphic Fault Zones,s ions in the grain boundary region. Gradients in activities of aqueous species (and chemical potential) can cause diffusive mass transfer (DMT) along the grain-boundary region. This causes the redistribution of chemical components and hence minerals in the rock.