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Gravity anomalies of 2D fault structures with fault planes described by polynomial functions of arbitrary degree

机译:具有任意平面多项式函数描述的断层平面的二维断层结构的重力异常

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摘要

Fault planes are often listric in nature rather than planar. In contrast to the existing conventional methods which assume planar surfaces for fault planes, a new technique is presented in the space domain to compute the gravity anomalies of 2D fault structures with non-planar fault planes. Polynomial functions are used to describe the fault planes. In addition, the density contrast within the structure is also assumed to be varying continuously with depth comprehending the geological settings of passive continental margins with concomitant basinal development. Both analytical and numerical approaches are used to derive the expression for the gravity anomaly of the structure. The method is exemplified with a synthetic fault model.
机译:断层本质上通常是李斯特形的,而不是平面的。与假定断层平面为平面的现有常规方法相反,在空间域中提出了一种新技术,用于计算具有非平面断层的二维断层结构的重力异常。多项式函数用于描述故障平面。此外,还假定结构内的密度对比随深度(包括被动陆缘的地质环境以及盆地的发育)而不断变化。分析和数值方法均用于导出结构重力异常的表达式。该方法以综合故障模型为例。

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