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  • 1
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0008(75-21)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 51 S.
    Series Statement: Paper / Geological Survey of Canada 75-21
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 92.1107
    In: Developments in palaeontology and stratigraphy
    Type of Medium: Monograph available for loan
    Pages: XIV, 424 S.
    ISBN: 0444882537
    Series Statement: Developments in palaeontology and stratigraphy 13
    Classification:
    Petrology, Petrography
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Dordrecht [u.a.] : Reidel [u.a.]
    Call number: G 8676
    Type of Medium: Monograph available for loan
    Pages: xi, 598 S.
    ISBN: 9027721165
    Series Statement: Quantitative geology and geostatistics
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 4
    Call number: SR 90.0008(67-14)
    In: Paper
    Type of Medium: Series available for loan
    Pages: V, 54 S.
    Series Statement: Paper / Geological Survey of Canada 67-14
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 5
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0008(89-9)
    In: Paper
    Type of Medium: Series available for loan
    Pages: V, 588 S.
    ISBN: 0660135922
    Series Statement: Paper / Geological Survey of Canada 89-9
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 6
    Call number: SR 90.0913(91)
    In: Memoires du BRGM
    Type of Medium: Series available for loan
    Pages: 491 S.
    Series Statement: Mémoires du BRGM 91
    Language: French
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 28 (1996), S. 1001-1015 
    ISSN: 1573-8868
    Keywords: multifractal measure ; fractal spectrum ; codimension ; binomial multiplicative cascade model
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract The interrelationships between two previously developed multifractal models are discussed. These are the Evertsz-Mandelbrot model developed on the basis of the multifractal spectrum f(α), and the Schertzer-Lovejoy model based on the codimension function C(γ) where α and γ represent Hölder exponent and field order, respectively. It is shown how these two models are interrelated: they are identical for values of γ within the range D−α(0)≤γ≤D−αmin. where D is the Euclidean dimension. For D−αmax≤γ≤D−α(0), however, f(α) remains a continuous function of α whereas C(γ) assumes constant value. In this respect, the fractal spectrum f(α) can provide more information about the multifractal measure than the codimension function C(γ). The properties of the two models are illustrated by application to the binomial multiplicative cascade model.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Natural resources research 5 (1996), S. 117-130 
    ISSN: 1573-8981
    Keywords: Fractal ; multifractal ; fractal measure ; data integration ; cluster dimension ; GIS ; mineral potential mapping
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Concepts of fractal/multifractal dimensions and fractal measure were used to derive the prior and posterior probabilities that a small unit cell on a geological map contains one or more mineral deposits. This has led to a new version of the weights of evidence technique which is proposed for integrating spatial datasets that exhibit nonfractal and fractal patterns to predict mineral potential. The method is demonstrated with a case study of gold mineral potential estimation in the Iskut River area, northwestern British Columbia. Several geological, geophysical, and geochemical patterns (Paleozoic-Mesozoic sedimentary and volcanic clastic rocks; buffer zones around the contacts between sedimentary rocks and Mesozoic intrusive rocks; a linear magnetic anomaly; and geochemical anomalies for Au and associated elements in stream sediments) were integrated with the gold mineral occurrences which have fractal and multifractal properties with a box-counting dimension of 1.335±0.077 and cluster dimension of 1.219±0.037.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Natural resources research 8 (1999), S. 27-35 
    ISSN: 1573-8981
    Keywords: Weights of evidence ; fuzzy set ; data-driven method ; knowledge-driven method ; mineral potential mapping ; fuzzy probability
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract This paper proposes a new approach of weights of evidence method based on fuzzy sets and fuzzy probabilities for mineral potential mapping. It can be considered as a generalization of the ordinary weights of evidence method, which is based on binary or ternary patterns of evidence and has been used in conjunction with geographic information systems for mineral potential mapping during the past few years. In the newly proposed method, instead of separating evidence into binary or ternary form, fuzzy sets containing more subjective genetic elements are created; fuzzy probabilities are defined to construct a model for calculating the posterior probability of a unit area containing mineral deposits on the basis of the fuzzy evidence for the unit area. The method can be treated as a hybrid method, which allows objective or subjective definition of a fuzzy membership function of evidence augmented by objective definition of fuzzy or conditional probabilities. Posterior probabilities calculated by this method would depend on existing data in a totally data-driven approach method, but depend partly on expert's knowledge when the hybrid method is used. A case study for demonstration purposes consists of application of the method to gold deposits in Meguma Terrane, Nova Scotia, Canada.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 24 (1992), S. 731-758 
    ISSN: 1573-8868
    Keywords: spatial factors ; autocorrelation ; crosscorrelation ; correlogram ; gridded data ; irregularly spaced data
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract Spatial factor analysis (SFA) is a multivariate method that determines linear combinations of variables with maximum autocorrelation at a given lag. This is achieved by deriving estimates of auto-/cross-correlations of the variables and calculating the corresponding eigenvectors of the covariance quotient matrix. A two-point spatial factor analysis model derives factors by the formation of transition matrixU comparing auto-/cross-correlations at lag “0,”R 0, with those at a specified lag “d,”R d, expressed asU d=R 0 −1 Rd. The matrixU d can be decomposed into its spectral components which represent the spatial factors. The technique has been extended to include three points of reference. Spatial factors can be derived from the relationship: $$\left[ {\begin{array}{*{20}c} {U_{d1} } \\ {} \\ {\begin{array}{*{20}c} {} \\ {} \\ \end{array} } \\ {U_{d2} } \\ \end{array} } \right] = \left[ {\begin{array}{*{20}c} {R_0 R_{d3} } \\ {} \\ {\begin{array}{*{20}c} {} \\ {} \\ \end{array} } \\ {R_{d3} R_0 } \\ \end{array} } \right]^{ - 1} \left[ {\begin{array}{*{20}c} {R_{d1} } \\ {} \\ {\begin{array}{*{20}c} {} \\ {} \\ \end{array} } \\ {R_{d2} } \\ \end{array} } \right]$$ where the factors ofU d1 andU d2 predict the relationships of the variables over three lag distances and orientations from matricesR d1,R d2, andR d3. Estimates of auto-/cross-correlation can be achieved using irregularly spaced or gridded data from experimental correlograms or function estimates determined from the experimental correlograms. The technique has applications in studies where several variables have different spatial ranges or zones of influence.
    Type of Medium: Electronic Resource
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