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dc.contributor.author Babadagli T.
dc.date.accessioned 2021-05-05T05:04:42Z
dc.date.available 2021-05-05T05:04:42Z
dc.date.issued 2002
dc.identifier https://www.elibrary.ru/item.asp?id=1276724
dc.identifier.citation Mathematical Geology, 2002, 34, 6, 647-670
dc.identifier.issn 0882-8121
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/28382
dc.description.abstract A previous method proposed to measure the fractal dimension of pore spaces is adapted and modified for 2-D fracture networks. The method relies on scanning a 2-D fracture network through successive straight lines from top to bottom and measuring the distance between two fractures. The fractal dimension is then obtained using the log-log plot of the feature size and the number of features for this particular size at different magnifications. It is shown in this study that the method proposed to measure the fractal dimension of porous structures can be applicable to 2-D fracture networks with some modifications after testing it on synthetic and natural fracture patterns. The method is simplified to be useful for practical applications in the fractal analysis of fracture networks. The results reveal that, on the basis of the direction of scanning lines, different fractal behavior and dimensions can be obtained indicating that 2-D fracture networks possess multifractal character. This approach takes into account the effect of fracture orientation on the fractal behavior and anisotropic nature of fracture networks as well as the fracture density, length, and spatial distribution.
dc.subject 2-D FRACTURE NETWORKS
dc.subject FRACTAL
dc.subject FRACTURE ORIENTATION
dc.subject FRACTURE DENSITY
dc.subject FRACTURE LENGTH
dc.subject SCANNING DIRECTION EFFECT ON FRACTAL DIMENSION
dc.title SCANLINE METHOD TO DETERMINE THE FRACTAL NATURE OF 2-D FRACTURE NETWORKS
dc.type Статья


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