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地质体中广泛存在着裂隙,它们是地质体中气液介质主要贮存的空间和运移通道.然而,极大部分断裂的分布具有不确定性.在对随机断裂分布基本参数研究的基础上,提出用非平稳态随机过程模拟断裂间隔.通过统计窗中断裂的量测,构造一个随机断裂网络Monte-Carlo模型.这一仿真技术为探索断裂在地质体中的分布,研究气液在地壳中赋存和运移提供了新的途径和方法
Geological bodies widely exist cracks, which are the main storage space and migration channel of gas-liquid medium in geological bodies. However, the distribution of the largest part of the fractures is uncertain. Based on the study of the basic parameters of random fracture distribution, A nonstationary stochastic process is proposed to simulate the fracture interval. A Monte Carlo model of a random fracture network is constructed by measuring the fracture in the statistical window. This simulation technique is to explore the distribution of fractures in geological bodies and to study the gas-liquid in the crust. Medium Occupation and Migration Provide New Approaches and Methods