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Titlebook: Mathematical Models of Sedimentary Processes; An International Sym Daniel F. Merriam (Jessie Page Heroy Professor of Book 1972 Springer Sc

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21#
發(fā)表于 2025-3-25 05:25:45 | 只看該作者
22#
發(fā)表于 2025-3-25 08:45:07 | 只看該作者
Dietrich Marsalloped are provided. It should be stressed that these papers are attempts to recapture a deep sense of the kind of science Galileo was creating. Other papers in 978-90-277-0891-5978-94-009-9799-8Series ISSN 1566-659X Series E-ISSN 2215-1974
23#
發(fā)表于 2025-3-25 12:10:07 | 只看該作者
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發(fā)表于 2025-3-25 19:49:30 | 只看該作者
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發(fā)表于 2025-3-25 21:38:57 | 只看該作者
26#
發(fā)表于 2025-3-26 02:29:43 | 只看該作者
The Semi-Markov Process as a General Sedimentation Model,on the theory of random walk. The resulting bed thickness is either exponentially or Gamma distributed. Gamma distributions seem to fit observed bed- thickness better than the lognormal distribution. The semi-Markov process may result in exponential or polymodal bed thickness distributions. Examples of both have been generated by simulation.
27#
發(fā)表于 2025-3-26 08:05:34 | 只看該作者
Mathematical Search Procedures in Facies Modeling in Sedimentary Rocks,inciples are illustrated in a facies study of Pennsylvanian carbonate rocks (from southeastern Utah) in which principal component analysis, Euclidean distance function, standardization, and weighted and unweighted pair-group methods, are among the classificatory schemes employed in facies construction.
28#
發(fā)表于 2025-3-26 11:25:31 | 只看該作者
Conditional Simulation of Sedimentary Cycles in Three Dimensions, are determined. To do this a maximum likelihood method is used. The most probable shape of lenses between boreholes for each group of contemporary lenses is determined. In this manner the problem is thus solved. The results are given as a set of thickness maps for successive groups of lenses and as cross sections.
29#
發(fā)表于 2025-3-26 15:53:30 | 只看該作者
30#
發(fā)表于 2025-3-26 19:08:54 | 只看該作者
Book 1972r, 1971. The symposium, co- sponsored by the International Association for Mathematical Geology, entertained the subject, "Mathematical Models of Sedimentary Processes. " The subject is most appropriate because sedimentologists have long been concerned with processes and mechanisms of sedi- ment dis
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