ROCK KRIGING WITH THE MICROSCOPE

dc.contributor.author	Voytekhovsky Y.L.
dc.contributor.author	Fishman M.A.
dc.date.accessioned	2022-02-03T04:39:24Z
dc.date.available	2022-02-03T04:39:24Z
dc.date.issued	2003
dc.identifier	https://elibrary.ru/item.asp?id=13445154
dc.identifier.citation	Mathematical Geology, 2003, 35, 4, 451-458
dc.identifier.issn	0882-8121
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34875
dc.description.abstract	An idea to consider rock textures from a geostatistical viewpoint is suggested. Mineral grains are coded by indicator functions. Four metrics are shown of interest for petrographic applications. The simplest one is used to calculate covariograms of indicators for platinum-bearing gabbronorite from the Pansky rock massif (Kola Peninsula, Russia) with maximal range of 2 units. This is generalized in the concept of a minimal cluster of mineral grains for the given rock. The theory allows us to combine grain-by-grain and cluster-by-cluster considerations of rock texture. It may be used to classify monotonous lithological series using nuances of rock textures.
dc.subject	rock texture
dc.subject	kriging
dc.subject	geostatistics
dc.subject	indicator function
dc.subject	metrics
dc.subject	mineral grain
dc.subject	gabbronorite
dc.title	ROCK KRIGING WITH THE MICROSCOPE
dc.type	Статья

Files in this item

Name: Voyt_03.pdf

Size: 86.76Kb

Format: PDF