(a) parameterize the geological reference horizon by linking to it a two-dimensional parametric system of paleogeographic coordinates;(b) construct a modeling function, the isovalue curves of which are approximately parallel to the general direction of the ancient riverbed to be simulated;(c) use the absolute value of the modeling function of the general direction of the ancient riverbed to be located in order to define a topographic function of the pseudo-valley;(d) transform the topographic function of the pseudo-valley by using a transfer function to determine the thicknesses, dimensions and characteristics of the ancient riverbed to be located and/or the ancient geological structures associated with this ancient riverbed."/> Process, device and package for stochastic simulation of ancient riverbeds or ancient geological structures
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Process, device and package for stochastic simulation of ancient riverbeds or ancient geological structures

机译：随机模拟古代河床或古代地质构造的工艺，装置和包装

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A process for stochastic simulation of ancient riverbeds or ancient geological structures includes the following stages:(a) parameterize the geological reference horizon by linking to it a two-dimensional parametric system of paleogeographic coordinates;(b) construct a modeling function, the isovalue curves of which are approximately parallel to the general direction of the ancient riverbed to be simulated;(c) use the absolute value of the modeling function of the general direction of the ancient riverbed to be located in order to define a topographic function of the pseudo-valley;(d) transform the topographic function of the pseudo-valley by using a transfer function to determine the thicknesses, dimensions and characteristics of the ancient riverbed to be located and/or the ancient geological structures associated with this ancient riverbed.
机译：古代河床或古代地质结构的随机模拟过程包括以下阶段： （a）通过将古地理坐标的二维参数系统链接到地质参考层来对其进行参数化; （b）构造一个建模函数，其等值曲线与要模拟的古代河床的大致方向大致平行; （c）使用绝对为了定义伪河谷的地形函数而要定位的古河床大方向的建模函数的值; （d ），通过使用传递函数来确定拟定位的古河床和/或古河床的厚度，尺寸和特征，从而对伪谷的地形函数进行变换与此古老河床相关的地质构造。

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