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A comparative study of natural and experimental nano-sized grinding grain textures in rocks

查看全文 作  者:SUN [1]Yan;SHU [1]LiangShu;LU [1]XianCai;LIU [1]Hao;ZHANG [2]XiHui;K. [3]KOSAKA;LIN [4]AiMing 高影响力作者 机构地区:[1]Department of Earth Sciences, State Key Laboratory for Research of Mineral Deposits, Nanjing University, Nanjing 210093, China;[2]Department of Management Information Systems, University of Memphis, Tennessee 38152, USA;[3]Department of Geosystem Sciences, Nihon University, Tokyo 156-8550, Japan;[4]Department of Geosciences, Shizuoka University, Shizuoka 422-8529, Japan高影响力机构 出  处:《Chinese Science Bulletin》索引2008年第53卷第8期,共5页高影响力期刊 基  金:the National Natural Science Foundation of China (Grant Nos. 40634022, 40673041, 40572118 and 40372092) ;the State Key Laboratory of Geology and Exploitation of Petroleum Reservoir (PLN 0606) 摘  要:In three shallow-level fault systems in eastern China, nano-sized (30―100 nm) grinding grain textures are found in the thin-shelled rheological layer representing frictional-viscous high strain field. The surface layer near slipping plane is composed of stacks of grinding grains with high sphericity and uniform nano-sized diameter, while the underlying layer appears as a mixture of irregular ones with diverse diameters. Rock deformation experiments indicate that the grinding grain texture is a common phenomenon in shearing fractures, suggesting a potential transition from sliding friction to rolling one during the rock deformation process. This transition is crucial for many tribological processes in geo- logical fields. 关 键 词:研磨颗粒结构 剪切薄板 摩擦粘性压力领域 岩石
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