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  • Articles  (9)
  • structure  (9)
  • 1975-1979  (9)
  • 1965-1969
  • 1945-1949
  • Geosciences  (9)
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 8 (1976), S. 183-202 
    ISSN: 1573-8868
    Keywords: Fourier analysis ; paleontology ; structure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract A system of strain analysis based on the application of a homogeneous strain transformation in plane polar coordinates to match deformed shapes of the same initial form is described. Two types of transformation are derived. A simple transformation between the deformed and the undeformed states, used to compare deformed shapes with a predetermined initial configuration, is recorded in the form of a plane polar coordinate Fourier series. This method allows reliable strain estimates to be made from single specimens of a fossil in an area where sufficient consistency of original shape has been established. A transformation describing the difference in relative strain between local polar coordinate systems in the same overall homogeneous deformation field, is used to compare the members of a group of deformed shapes with one another. This transformation allows the determination of the optimum initial ‘mean shape’of a group of fossils in a deformed rock as well as giving a strain measurement. The use of parabolic integration enhances the determination of the Fourier descriptions, and allows the use of irregularly spaced data. Inherent mathematical features of the method provide controls on the accuracy of the determination. The relatively mechanical nature of the input and the general form of the solution make the method readily applicable in semiautomated systems.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 8 (1976), S. 9-23 
    ISSN: 1573-8868
    Keywords: cluster analysis ; statistics ; numerical taxonomy ; structure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract This paper presents a technique for (1) clustering orientation data with minimum constraint on resulting partitions, and (2) testing clusters against a probability distribution defined on the unit sphere which admits elliptical symmetry about its mean. The use of an objective function to highlight certain features of the data is discussed. The technique for delineation and analysis of clusters is applied to an example problem through use of a computer code.
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 7 (1975), S. 285-293 
    ISSN: 1573-8868
    Keywords: cluster analysis ; data processing ; orientation data ; statistics ; structure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract A method of cluster analysis for orientation data is described. The method enables vector statistics to be applied to polymodal distributions. Similar results to those found by modal analysis are obtained.
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 7 (1975), S. 295-321 
    ISSN: 1573-8868
    Keywords: data processing ; data structure ; independent events ; paleontology ; petrology ; regional mapping ; stratigraphy ; structure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract Geological events, such as emplacement of granite or growth of slaty cleavage, may be ordered into a sequence by two methods. One is to assign each event a place in a time scale, such as years before the present, which amounts to assigning events an age designation from the set of real numbers. In ordering such a list, the algebra of real numbers applies. A second method is to determine the time relations of events in pairs, such as a fold is of type (S1, S2) or granite intrudes conglomerate. These binary relations between events may be used to order events into a sequence using the transitive properties of the relation “older than.” It is shown, however, that the binary relations between events do not follow the familiar rules for the algebra of real or integral numbers and it is necessary to erect a new system of relations called the “algebra of events.” The fundamental relation is “older than or equivalent to” and this may be used to define the relations “older than”, “younger than”, “equivalent to”, “incomparable to”, and “covers.” The essential difference from the algebra of integers is that the reflexive relation (“equal to”) is replaced by two such relations (“equivalent to” and “incomparable to”) in the algebra of events. A number of binary relations between events may be assembled into an event matrix which is basically a truth table for the relation “older than.” This may be ordered and stacked by operations termed ORDER and STACK. The relationship of each event to every other event may be determined by simple inspection of an ordered, stacked matrix, and from this a geological history may be assembled. If there are contradictions in the field data, ordering into a proper sequence is impossible and may be detected. If there are ambiguities in the field data, there are several different orders that are proper sequences so that the event matrix may be ordered. However, the ambiguities occur as voids in the stacked matrix.
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 7 (1975), S. 373-394 
    ISSN: 1573-8868
    Keywords: bias ; data density ; graphics ; machine contouring ; mapping ; sampling ; exploration ; petroleum ; structure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract Contouring of data by men and machines produces a collection of maps which demonstrates differences between them; exploration geologists, computer-mapping-package-builders, and managers should be aware of these differences. Machines and geologists contouring subsurface structural data were compared in terms of the ultimate accuracy of their maps. The machine versions were consistently more similar to the carbonate reef surface used for the analysis than those produced by the geologists, given specific amounts of control. However, in situations where additional information was critical (paleoslope, channel vs bar sand, regional dip, etc.) the bias contributed by the geologist proved critical to the “correct” interpretation. Several illustrations in the form of actual exploration examples are included and discussed. The examples described and analyzed herein are presented to acquaint both the map-maker and map-user with each other's problems with the overall objective of increasing the explorational effectiveness of both.
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 8 (1976), S. 375-393 
    ISSN: 1573-8868
    Keywords: digitization ; graphics ; mapping ; plotting ; data bank ; stratigraphy ; structure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract A method is presented which describes rational digitization and efficient treatment of a geologic map. An oriented graph, S,the arcs of which are associated with stratigraphic boundaries and imply a difference in the topological nature of the map if it includes faults, is used. From S,we deduce other graphs: a dendrogram which is used to structure the data and a graph which summarizes the geologic properties of the map. This structure is useful for graphic reconstitutions on a plotter or screen, and for quantitative correlation and calculation of dips, surfaces, and volumes.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 8 (1976), S. 549-559 
    ISSN: 1573-8868
    Keywords: cylindrical folds ; orientation data ; statistics ; Bingham's distribution ; structure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract An asymptotic form of Bingham's distribution on the sphere is applied to orientation data from cylindrical folds. Data from cylindrical folds typically form two clusters, one cluster for each fold limb. A bimodal distribution is obtained by fitting a unimodal distribution to each cluster. One parameter of the distribution gives the fold axis, another parameter is directly related to the curvature of the fold limb. Certain tests of hypotheses based on this distribution are the same as tests based on the Dimroth—Watson (symmetric girdle)distribution. One such is the test of whether two folds have the same fold axis.
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 8 (1976), S. 649-655 
    ISSN: 1573-8868
    Keywords: topology ; catastrophe theory ; volcanology ; sedimentology ; structure ; morphogenesis
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract Catastrophe theory is a recently developed branch of topology which has a number of practical applications, principally because of its ability to model situations which include discontinuities or singularities, where the methods of differential calculus break down. Some examples of its possible use in geology are presented, in fields as diverse as volcanology, sedimentology, and structural geology, and wider applications, in modeling spatial or temporal discontinuities in other fields, are suggested.
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Mathematical geology 9 (1977), S. 3-38 
    ISSN: 1573-8868
    Keywords: optical processing ; Fourier analysis ; structure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract Optical processing is a fast, easy, economical, and reliable method of quantifying map patterns. A reduced transparency of a zebra-like pattern, obtained by blackening in alternate contour bands of a map, is used as input to an optical system of a laser source and objective lens to produce Fourier transforms. By sampling the intensity distribution across the transform, information about the spatial frequency (periodicity) and orientation in the original map can be inferred. Parameters used for comparing the map images are the values of intensity distribution in the transform. These intensities are normalized and subjected to comparison using various similarity methods. Cross-multiplication of the intensities is suggested as a measure of vectorial comparison of the orientations. By plotting the directional intensities into a polar coordinate system, rose diagrams are prepared for visual comparison. Optically derived parameters are independent of scale and other restrictive and limiting requirements as demanded in techniques of map analyses based on numerically derived parameters. The technique can be used in analyzing other pictorial data including aerial photographs, rock-fabric diagrams, and thin sections.
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