A New Method to Select Training Images in Multi-Point Geostatistics

Abstract

Training images, as an important modeling parameter in the multi-point geostatistics, directly determine the effect of modeling. It's necessary to evaluate and select the candidate training image before using the multi-point geostatistical modeling. The overall repetition probability is not sufficient to describe the relationship of single data events in the training image. Based on the understanding, a new method was presented in this paper to select the training image. As is shown in the basic idea, the repetition probability distribution of a single data event was used to characterize the type and stationarity of the sedimentary pattern in the training image. The repetition probability mean value and deviation of single data event reflected the stationarity of the geological model of the training image; the rate of data event mismatching reflected the diversity of geological patterns in training images. The selection of optimal training image was achieved by combining the probability of repeated events and the probability of overall repetition of single data events. It's illustrated in the simulation tests that a good training image has the advantages of high repetition probability compatibility, stable distribution of repeated probability of single data event, low probability mean value, low probability deviation and low rate of mismatching. The method can quickly select the training image and provide the basic guarantee for multi-point geostatistical simulations.

Avaliação de diferentes medidas de similaridade no SIMDISPAT - Novo Algoritmo de Simulação de Múltiplos Pontos

“…Além disso, este modelo proporciona uma imagem única das características geológicas. Os recentes avanços nos métodos de mapeamento de afloramentos são digitais, incluindo fotogrametria, que permite a rápida aquisição de modelos 3 de afloramentos virtuais de alta resolução (WANG et al, 2018). Finalmente, a terceira forma de construir apresentada em Tahmasebi (2018), são métodos baseados em processos, que apresentam uma maneira de representar uma heterogeneidade geológica realista em modelos de subsolo, que pretendem desenvolver modelos 3 de um meio poroso.…”