2017
DOI: 10.3390/min7120241
|View full text |Cite
|
Sign up to set email alerts
|

Indicator Variograms as an Aid for Geological Interpretation and Modeling of Ore Deposits

Abstract: Geostatistics offers a set of methods for modeling, predicting, or simulating geological domains in space. In addition of being an input of some of these methods, indicator direct and cross-variograms convey valuable information on the geometry of the domain layouts and on their contact relationships, in particular, on the surface area of a domain boundary, on the surface area of the contact between two domains, on the propensity for a domain to be in contact with, or separated from, another domain, and on the… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
7
0

Year Published

2018
2018
2024
2024

Publication Types

Select...
8
1

Relationship

0
9

Authors

Journals

citations
Cited by 15 publications
(7 citation statements)
references
References 33 publications
(32 reference statements)
0
7
0
Order By: Relevance
“…It is also worth mentioning that anisotropy was examined through the original dataset (not transformed), and it was seen that the existence of anisotropy in the region was improbable. For fitting of theoretical variograms over experimental variograms, the linear model of co-regionalization [45] with semi-automatic technique is chosen, in which the semi-definiteness condition [36,46] is respected through the process of fitting. In this model, direct and cross-covariances are defined as the sum of basic covariances.…”
Section: Variogram Inferencementioning
confidence: 99%
“…It is also worth mentioning that anisotropy was examined through the original dataset (not transformed), and it was seen that the existence of anisotropy in the region was improbable. For fitting of theoretical variograms over experimental variograms, the linear model of co-regionalization [45] with semi-automatic technique is chosen, in which the semi-definiteness condition [36,46] is respected through the process of fitting. In this model, direct and cross-covariances are defined as the sum of basic covariances.…”
Section: Variogram Inferencementioning
confidence: 99%
“…To do so, experimental variogram (ℎ) computes the average dissimilarity between data separated by vector ℎ. It is calculated as half the average squared difference between the components of every data pair [10,35]:…”
Section: Modeling Spatial Continuity: Variogram Analysismentioning
confidence: 99%
“…Spatial continuity of geological properties including geomechanical parameters can be a measure of changes in variance versus distance. To do so, experimental variogram γ(h) computes the average dissimilarity between data separated by vector h. It is calculated as half the average squared difference between the components of every data pair [10,35]:…”
Section: Modeling Spatial Continuity: Variogram Analysismentioning
confidence: 99%
“…Lithotypes are classified into different categories based on interclass dependencies. However, the following two issues, among others, occur during lithotype modeling in an ore deposit 3 . The first one is defining domain layout to minimize misclassifications.…”
Section: Introductionmentioning
confidence: 99%