ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Keywords: Earth sciences ; Geology ; Statistical methods ; Mathematical physics ; Statistics ; Earth Sciences ; Quantitative Geology ; Mathematical Applications in the Physical Sciences ; Statistics for Engineering, Physics, Computer Science, Chemistry and Earth Sciences ; Statistics and Computing/Statistics Programs ; Applications of Nonlinear Dynamics and Chaos Theory
    Description / Table of Contents: 1. Forward --- 2. Preface --- 3. Introduction --- 4. Part I. Chapter 1 Kriging, Splines, Conditional Simulation, Bayesian In-version and Ensemble Kalman Filtering --- 5. Chapter 2 A Statistical Commentary on Mineral Prospectivity analysis --- 6. Chapter 3 Testing joint conditional independence of categorical random variables with a standard log-likelihood ratio test --- 7. Chapter 4 Modelling Compositional Data. The Sample Space Approach --- 8. Chapter 5 Properties of Sums of Geological Random Variables --- 9. Chapter 6 A Statistical Analysis of the Jacobian in Retrievals of Satellite Data --- 10. Chapter 7 All Realizations All the Time --- 11. Chapter 8 Binary Coefficients Redux --- 12. Chapter 9 Tracking Plurigaussian Simulations --- 13. Chapter 10 Mathematical Geosciences: Local Singularity Analysis of Nonlinear Earth Processes and Extreme Geo-Events --- 14. Chapter 11 Electrofacies in Reservoir Characterization --- 15. Chapter 12 Forecast of Shoreline Variations by Means of Median Sets --- 16. Chapter 13 An Introduction to the Spatio-Temporal Analysis of Sat-ellite Remote Sensing Data for Geostatisticians --- 17. Chapter 14 Flint drinking water crisis: a first attempt to model geo-statistically the space-time distribution of water lead levels --- 18. Chapter 15 Statistical Parametric Mapping for Geoscience Applications --- 19. Chapter 16 Water chemistry: are new challenges possible from CoDA (Compositional Data Analysis) point of view? --- 20. Chapter 17 Analysis of the United States Portion of the North American Soil Geochemical Landscapes Project – A Compositional Framework Approach --- 21. Chapter 18 Quantifying the Impacts of Uncertainty --- 22. Chapter 19. Advances in Sensitivity Analysis of Uncertainty due to Sampling Density for Spatially Correlated Attributes --- 23. Chapter 20 Predicting Molybdenum Deposit Growth --- 24. Chapter 21 General Framework of Quantitative Target Selections --- 25. Chapter 22 Solving the Wrong Resource Assessment Problems Precisely --- 26. Chapter 23 two ideas for analysis of multivariate geochemical survey data: proximity regression and principal component residuals --- 27. Chapter 24 Mathematical minerals: A history of petrophysical petrography --- 28. Chapter 25 Geostatistics for Seismic Characterization of Oil Reservoirs --- 29. Chapter 26 Statistical Modeling of Regional and Worldwide Size-Frequency Distributions of Metal Deposits --- 30. Chapter 27 Bayesianism in the Geosciences --- 31.Chapter 28 Geological Objects and Physical Parameter Fields in the Subsurface: A Review --- 32.Chapter 29 Fifty Years of Kriging --- 33. Chapter 30 Multiple Point Statistics: A Review --- 34. Chapter 31 When Should We Use Multiple-Point Geostatistics? --- 35. Chapter 32 The Origins of the Multiple-Point Statistics (MPS) Algorithm --- 36. Chapter 33 Predictive Geometallurgy: An Interdisciplinary Key Challenge for Mathematical Geosciences? --- 37. Chapter 34 Data Science for Geoscience: Leveraging Mathematical Geosciences with Semantics and Open Data --- 38. Chapter 35 Mathematical Morphology in Geosciences and GISci: An Illustrative Review --- 39. Chapter 36 IAMG: Recollections from the Early Years --- 40. Chapter 37 Forward and Inverse Models over 70 Years --- 41. Chapter 38 From individual personal contacts 1962–1968 to my 50 years of service --- 42. Chapter 39 Andrey Borisovich Vistelius --- 43. Chapter 40 Fifty Years’ Experience with Hidden Errors in Applying Classic Mathematical Geology --- 44. Chapter 41 Mathematical Geology by Example: Teaching and Learning Perspectives.
    Pages: Online-Ressource (XXVIII, 914 pages) , 287 illustrations, 185 illustrations in color
    ISBN: 9783319789996
    Language: English
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    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
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    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
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Natural resources research 9 (2000), S. 43-52 
    ISSN: 1573-8981
    Keywords: Spatial analysis ; spectrum analysis ; geochemical data analysis ; GIS ; multifractal modeling ; soil sample
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract A new approach for separating geochemical anomalies from background has been developedon the basis of integration of spatial and spectrum analysis. A map generated from geochemicaldata can be transformed into a frequency domain in which a spatial concentration-area fractalmethod can be applied to distinguish the patterns on the basis of the power-spectrum distribution.Distinct classes can be generated, such as lower, intermediate, and high power-spectrum valuesapproximately corresponding to background, anomalies, and noises of geochemical values ina spatial domain. An irregular filter then can be constructed on these distinct patterns withthe background and noises related to low- and high-power-spectrum values being removed.The image converted back to a spatial domain with the filter applied can show patterns which,after the removal of background and noise, mainly reflect a residual area that representsanomalous or atypical geochemical patterns. This method is demonstrated using a case studyof soil geochemical data from the Mudik area, on the island of Sumatra, Indonesia. The resultsobtained from this method in comparison with those obtained from other methods have shownthat the newly developed method can separate overlapping populations without using a singlecutoff value.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Natural resources research 5 (1996), S. 169-180 
    ISSN: 1573-8981
    Keywords: Fuzzy relation ; partial order relation ; asymmetric incidence coefficient ; probability difference ; double sampling ; mineral resource prediction
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract A fuzzy relation analysis method is used to derive weights for qualitative variables based on their partial order relations. Two asymmetric measure indexes (incidence coefficient and probability difference) are proposed to measure the asymmetric associations between geoscience variables from which the partial order relations can be constructed. The fuzzy relation analysis method can be implemented in combination with the asymmetric measure indexes leading to new methods for pattern overlay and data integration in mineral potential prediction. Two types of models are proposed and illustrated by two artificial examples: one for predicting targets for undiscovered deposits, and the other for estimating the mineral resource potential of the targets.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    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
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 29 (1997), S. 919-932 
    ISSN: 1573-8868
    Keywords: multifractals ; fractal ; lacunarity ; gliding box ; box-counting ; moments
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract The so-called “gliding box method” of lacunarity analysis has been investigated for implementing multifractal modeling in comparison with the ordinary box-counting method. Newly derived results show that the lacunarity index is associated with the dimension (codimension) of fractal, multifractal and some types of nonfractals in power-law relations involving box size; the exponent of the lacunarity function corresponds to the fractal codimension (E – D) for fractals and nonfractals, and to the correlation codimension (E – τlpar;2)) for multifractals. These results are illustrated with two case studies: De Wijs's zinc concentration values from the Pulacayo sphalerite-quartz vein in Bolivia and Cochran's tree seedlings example. Both yield low lacunarities and slightly depart from translational invariance.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 31 (1999), S. 455-469 
    ISSN: 1573-8868
    Keywords: discrete multifractals ; Markov processes ; multiplicative cascade processes ; Carlin type gold deposits ; Nevada
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract Fractals and multifractals are a natural consequence of self-similarity resulting from scale-independent processes. Multifractals are spatially intertwined fractals which can be further grouped into two classes according to the characteristics of their fractal dimension spectra: continuous and discrete multifractals. The concept of multifractals emphasizes spatial associations between fractals and fractal spectra. Distinguishing discrete multifractals from continuous multifractals makes it possible to describe discrete physical processes from a multifractal point of view. It is shown that multiplicative cascade processes can generate continuous multifractals and that Markov processes result in discrete multifractals. The latter result provides not only theoretical evidence for existence of discrete multifractals but also a fundamental model illustrating the general properties of discrete multifractals. Classical prefractal examples are used to show how asymmetrical Markov process can be applied to generate prefractal sets and discrete multifractals. The discrete multifractal model based on Markov processes was applied to a dataset of gold deposits in the Great Basin, Nevada, USA. The gold deposits were regarded as discrete multifractals consisting of three spatially interrelated point sets (small, medium, and large deposits) yielding fractal dimensions of 0.541 for the small deposits (〈25 tons Au), 0.296 for the medium deposits (25--500 tons Au), and 0.09 for the large deposits (〉500 tons Au), respectively.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 27 (1995), S. 69-82 
    ISSN: 1573-8868
    Keywords: similarly shaped geometries ; fractal dimension ; area ; perimeter ; volume ; power-law relation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract Perimeters and areas of similarly shaped fractal geometries in two-dimensional space are related to one another by power-law relationships. The exponents obtained from these power laws are associated with, but do not necessarily provide, unbiased estimates of the fractal dimensions of the perimeters and areas. The exponent (DAL) obtained from perimeter-area analysis can be used only as a reliable estimate of the dimension of the perimeter (DL) if the dimension of the measured area is DA=2. If DA〈2, then the exponent DAL=2DL/DA〉DL. Similar relations hold true for area and volumes of three-dimensional fractal geometries. The newly derived results are used for characterizing Au associated alteration zones in porphyry systems in the Mitchell-Sulphurets mineral district, northwestern British Columbia.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 28 (1996), S. 1-16 
    ISSN: 1573-8868
    Keywords: autocorrelation ; fractals ; mass exponents ; multifractal spectrum ; semivariogram ; spatial covariance
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract In general, the multifractal model provides more information about measurements on spatial objects than a fractal model. It also results in mathematical equations for the covariance function and semivariogram in spatial statistics which are determined primarily by the second-order mass exponent. However, these equations can be approximated by power-law relations which are comparable directly to equations based on fractal modeling. The multifractal approach is used to describe the underlying spatial structure of De Wijs 's example of zinc values from a sphalerite-bearing quartz vein near Pulacayo, Bolivia. It is shown that these data are multifractal instead of fractal, and that the second-order mass exponent (=0.979±0.011 for the example) can be used in spatial statistical analysis.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...