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A mechanical-statistical model is presented that aims to help to understand the history and geometry of the process of formation of fracture zones along oceanic ridges. It uses ideas of statistical fracture theory used in engineering, namely the Weibull fracture model. The approximate parallelism of the fracture zones along ridges makes it possible to use a one-dimensional point process model with points along the ridge axes, which represent the transform faults. The ratios of the lengths of the corresponding fracture zones to the ocean width are used to obtain a rough estimate of the Weibull modulus, which is an important material parameter in fracture theory. The theory is refined by introducing a hard-core point process model. The corresponding positive minimum distance between subsequent fracture zones results from stress relaxation in the vicinity of a given fracture zone.  相似文献   

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Present-day tectonic concepts of events on the western paleo-Pacific lithosphere must be assessed relative to new data. Data collected by the newer techniques of geophysical surveying reveal leaky fracture zones, trending NNW–SSE and WSW–ENE; non-sequential in-line ages on most seamount chains; and orthogonal intersections of fracture zones. The fracture zones meander, braid, merge, splay, start and stop at any place, and are generally aligned with, or contain, linear chains of seamount. The combination of these in-line features is called megatrends. When the GEOSAT data are compared to the available bathymetry, this seemingly jumbled tectonic structure is verified. As the pole of rotation changes, the stress field changes alignment to agree with the Chandler wobble of Earth. Younger megatrends, propagating ever eastward, cross the older, already imprinted megatrends. During the Cretaceous, the voluminous outpouring of igneous rock created the large Pacific plateaus and rises where the megatrends, active and inactive, orthogonally intersected. The magma floods at the intersections flowed outwardly, and the outward flooding accounts for the fanning magnetic lineations around the Manihiki, Magellan, Shatskiy, and Hess rises. A case study of the Mid-Pacific Mountains (MPM), lying in the north-central Pacific Ocean basin, shows that the MPM formed about 125–110-Ma by overprinting the orthogonal intersections of fracture zones at the Molokai and Easter/Krusenstern–Emperor megatrends and the Murray and Tubai/Mamua megatrends. The MPM have been undergoing distortion into a vortex structure, a feature which has been confirmed by updated bathymetry, GEOSAT altimetry data, and drillsite information.  相似文献   

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本文运用断裂力学的原理和方法,分析了斜坡破坏过程中后缘开裂、滑动面的形成和结构面连通的机理,以及破坏中所遵循的轨迹。通过模拟实验、数值分析和应用,证明断裂力学方法是一种分析斜坡破坏机理的有效方法。  相似文献   

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目的 探讨L形切口治疗闭合性跟骨骨折的术后疗效及影响因素分析。方法 采用回顾性分析研究方法,收集笔者医院自2010年1月~2015年1月收治并行外侧L形切口切开复位内固定术治疗闭合性跟骨骨折的患者临床资料,共150例,其中SandersⅡ、Ⅲ、Ⅳ型各50例,观察术前、术后Bohler角和Gissane角度变化值,术后切口并发症,随访术后Maryland足部评分标准,对可能影响患者术后切口并发症相关变量进行单因素分析,对差异有统计学意义的变量进行多因素Logistic 回归分析。结果 所有患者均完成术后随访,随访时间12~24个月,平均随访时间17个月,以Maryland评分标准进行足部功能评估,优良率为79%,术后切口并发症为16%。结论 L形切口治疗闭合性跟骨骨折SandersⅡ~Ⅳ术后优良率较高,探索影响术后切口并发症的相关因素,发现吸烟、糖尿病、手术时长、受伤至手术时间可使术后切口并发症增加。  相似文献   

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