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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Simulating brittle fault growth from linkage of preexisting structures
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Simulating brittle fault growth from linkage of preexisting structures

机译:通过现有结构的链接模拟脆性断层的增长

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摘要

Many researchers have proposed conceptual models of fault development that are based on the linkage of preexisting structures such as isolated faults, joints or veins. To date, such models largely use theoretical mechanics to explain the detailed damage zone geometries observed in linkage structures. In this paper, we present the first numerical simulations of the temporal and spatial development of geometrically complex fault linkage structures using the finite element model for fault damage zone evolution, MOPEDZ. Simulations show spatial and temporal fault zone evolution for a range of preexisting joint (or fault) geometries and stress conditions. Simulations show that linkage geometries are governed by three key factors: the stress ratio; the original joint geometry, such as contractional or dilational configurations; and the orientation of the principal stress. Simulated linkage structures display close correspondence to field observations of fault zone geometry, with all secondary and tertiary damage features being reproduced. The research also demonstrates that given information on the regional stress conditions, numerical modeling can be used to predict fault zone geometries, and hence, identify the most (and least) likely structures for promoting fluid flow.
机译:许多研究人员已经提出了断层发育的概念模型,这些模型基于先前存在的结构(如孤立断层,关节或静脉)的联系。迄今为止,此类模型主要使用理论力学来解释在连杆结构中观察到的详细损伤区域几何形状。在本文中,我们使用故障破坏区域演化的有限元模型MOPEDZ,对几何复杂的断层连接结构的时空发展进行了首次数值模拟。仿真显示了一系列先前存在的接头(或断层)几何形状和应力条件的时空断层带演化。仿真表明,连杆机构的几何形状受三个关键因素控制:应力比;原始的关节几何形状,例如收缩或扩张构造;和主应力的方向。模拟的联动结构显示出与断层带几何形状的现场观测结果非常接近的对应关系,并复制了所有次生和三次生破坏特征。这项研究还表明,给定有关区域应力条件的信息,可以使用数值模型来预测断层带的几何形状,从而确定最(和最少)可能的结构来促进流体流动。

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