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新疆东部甘肃西部两种断裂体制及其推覆构造
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作者 张朝文 《成都地质学院学报》 CSCD 1993年第3期39-45,共7页
地质、地球物理测深研究成果揭示新疆东部、甘肃西部存在两个世代、两种不同的断裂体制:深部断裂体制,形成于古生代,主要反映板块碰撞-对接前板块之间或板内不同块段之间的离散与聚合,控制古生代的构造格局;浅部断裂体制,形成于华力西... 地质、地球物理测深研究成果揭示新疆东部、甘肃西部存在两个世代、两种不同的断裂体制:深部断裂体制,形成于古生代,主要反映板块碰撞-对接前板块之间或板内不同块段之间的离散与聚合,控制古生代的构造格局;浅部断裂体制,形成于华力西晚期至中新生代,主要反映板块碰撞-对接后壳内强烈水平挤压,控制中新生代构造格局或逆冲-推覆-滑脱构造。 展开更多
关键词 断裂体制 推覆构造 新疆 构造格局
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Macro-meso fracture evolution mechanism of hollow cylindrical granite with different hole diameters under conventional triaxial compression
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作者 ZENG Lin-hai ZHANG Dao-bing +2 位作者 ZHANG Jia-hua ZHANG Biao YIN Hua-dong 《Journal of Central South University》 SCIE EI CAS CSCD 2024年第9期3281-3294,共14页
In order to study and analyze the stability of engineering rock mass under non-uniform triaxial stress and obtain the evolution mechanism of the whole process of fracture,a series of conventional triaxial compression ... In order to study and analyze the stability of engineering rock mass under non-uniform triaxial stress and obtain the evolution mechanism of the whole process of fracture,a series of conventional triaxial compression tests and three-dimensional numerical simulation tests were carried out on hollow granite specimens with different diameters.The bearing capacity of hollow cylindrical specimen is analyzed based on elasticity.The results show that:1)Under low confining pressure,the tensile strain near the hole of the hollow cylindrical specimen is obvious,and the specimen deformation near the hole is significant.At the initial stage of loading,the compressive stress and compressive strain of the specimen are widely distributed.With the progress of loading,the number of microelements subjected to tensile strain gradually increases,and even spreads throughout the specimen;2)Under conventional triaxial compression,the cracking position of hollow cylinder specimens is concentrated in the upper and lower parts,and the final fracture mode is generally compressive shear failure.The final fracture mode of complete specimen is generally tensile fracture.Under high confining pressure,the tensile cracks of the sample are concentrated in the upper and lower parts and are not connected,while the cracks of the upper and lower parts of the intact sample will expand and connect to form a fracture surface;3)In addition,the tensile crack widths of intact and hollow cylindrical specimens under low confining pressure are larger than those under high confining pressure. 展开更多
关键词 hollow-cylinder granite fracture mechanism hole size compressed deformation crack propagation
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