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Titlebook: Geologic Modeling and Mapping; Andrea Förster,Daniel F. Merriam Book 1996 Plenum Press, New York 1996 Ordovician.Sediment.diagenesis.geolo

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书目名称Geologic Modeling and Mapping
编辑Andrea Förster,Daniel F. Merriam
视频video
丛书名称Computer Applications in the Earth Sciences
图书封面Titlebook: Geologic Modeling and Mapping;  Andrea Förster,Daniel F. Merriam Book 1996 Plenum Press, New York 1996 Ordovician.Sediment.diagenesis.geolo
描述This volume is a compendium of papers on the subject, as noted in the book title, of modeling and mapping. They were presented at the 25th Anniversary meeting of the International Association for Mathematical Geology (IAMG) at Praha (Prague), Czech Republic in October of 1993. The Association, founded at the International Geological Congress (IGC) in Prague in 1968, returned to its origins for its Silver Anniversary celebration. All in all 146 papers by 276 authors were offered for the 165 attendees at the 3-day meeting convened in the Hotel Krystal. It was a time for remembrance and for future prognostication. The selected papers in Geologic Modeling and Mapping comprise a broad range of powerful techniques used nowadays in the earth sciences. Modeling stands for reconstruction of geological features, such as subsurface structure, in space and time, as well as for simulation of geological processes both providing scenarios of geologic events and how these events might have occurred. Mapping stands for spatial analysis of data, a topic that always has been an extremely important part of the earth sciences. Because both modeling and mapping are used widely in conjunction, the book t
出版日期Book 1996
关键词Ordovician; Sediment; diagenesis; geology; geoscience; modeling; modelling; reservoir; sedimentary basin; tra
版次1
doihttps://doi.org/10.1007/978-1-4613-0363-3
isbn_softcover978-1-4613-8017-7
isbn_ebook978-1-4613-0363-3Series ISSN 1567-8296
issn_series 1567-8296
copyrightPlenum Press, New York 1996
The information of publication is updating

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978-1-4613-8017-7Plenum Press, New York 1996
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Geologic Modeling and Mapping978-1-4613-0363-3Series ISSN 1567-8296
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https://doi.org/10.1007/978-3-642-91372-3perties are strongly influenced by lithology and facies distribution that stem from the geologic processes that generated them. Three types of simulators are contrasted that represent variations of petrophysical properties: stochastic simulators, stratigraphic-form simulators, and sedimentary proces
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,Die physikalischen Zusammenhänge,cipitation. The model includes various mineralogical components and dissolved species which are major components of many sandstones. The model allows the simulation of temporal and spatial evolution of porosity and mineral distribution in a sandstone layer. Possible application to diagenetic problem
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https://doi.org/10.1007/978-3-663-01906-0By necessity, petroleum reservoir prediction and modeling must make both interpolations and extrapolations from limited data. Several approaches to modeling of sedimentary rocks include descriptive or conceptual (qualitative) geologic models and geostatistical, simulation (process), and visualizatio
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Die molekulare Kardiologie bei Frauen,dy attempts to illustrate how the various factors may interact and how they may modify the thermal field. The main result focusses on the uncertainties related to the extrapolation from the near-surface field into greater depth. It is shown that a unique solution may not be guaranteed. However, the
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H. J. Engel,E. Engel,K. Behnke,P. Lichtlenir “effective” transport coefficients. It is shown that means and power laws provide empirical descriptions for the transport tensor and relate it to statistical measurements of the composition and structure of the medium. General anisotropic media are related to statistically isotropic media. The i
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,Homologie und Heterologie der Geschwülste,bility of high performance techniques for data handling, 2D and 3D interpolation and computer graphics. Under control of a programmable interface, commercial programs (ONTOS, GMP) and research developments (GEOSTORE, GRAPE, GOCAD) have been implemented in a workstation network using Remote Procedure
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https://doi.org/10.1007/978-3-642-91793-6f contour lines, which may represent the intersection of its boundary surface(s) with the plane of the cross section thus distinguishing the body’s interior and exterior, or a given value of some property of the body. Graphically displaying the body’s geometry and topology, that is its internal stru
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