By Raymond A. Price
About The Product
Published by means of the yank Geophysical Union as a part of the Geophysical Monograph Series.
The starting place and evolution of sedimentary basins is an seen concentration of the overseas Lithosphere software since it is essentially an issue within the dynamics and evolution of the lithosphere, and in addition, it presents specified possibilities for strengthening the interactions among uncomplicated examine and the functions of geology, geophysics, geochemistry and geodesy to mineral and effort exploration and improvement. consequently, at either the XXVIIth foreign Geological Congress in Moscow, in 1984, and on the XIXth normal meeting of the overseas Union of Geodesy and Geophysics in Vancouver, in 1987, the foreign Lithosphere software convened exact symposia just about the beginning and evolution of sedimentary basins and their mineral and effort assets. This exact quantity provides the various significant result of these symposia.
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In regards to the ProductPublished by way of the yank Geophysical Union as a part of the Geodynamics SeriesContent:
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Extra resources for Origin and Evolution of Sedimentary Basins and Their Energy and Mineral Resources
This solution can be extended to more complicated sea-level histories using standard Fourier-series techniques. Variable Time Lag Between Shoreline and Eustatic Oscillations It is of interest to understand how much can vary by, from one passive margin to another. As Geophysical Monograph Series Origin and Evolution of Sedimentary Basins and Their Energy and Mineral Resources TRANSGRESSIONS AND REGRESSIONS 32 Eustatic Sea Level 2T Ah 0 -Ah T Fig. 3. Displacement of shoreline from equilibrium position, caused by a sinusoidal eustatic oscillation of period T and amplitude Ah (from Equation 4).
Geophys. , 88, 10439-10447, 1983. , and K. Lambeck, Comments on thermal isostasy, J. , 2, 51-65, 1985. D. H. Pilger, Thermal evolution of the North-Central Gulf Coast, Tectonics, 3, 723-740, 1984. , A physical model for the creation of the lithosphere, Geophys. J. R. Astron. , 43, 425-451, 1975. , John-Wiley and Sons, New York, 1980. L. W. Oldenburg, Thermal model of ocean ridges, Nature Phys. , 242, 137-139, 1973. Parsons, B. G. Sclater, An analysis of the variation of ocean floor bathymetry and heat flow with age, J.
Summary and Conclusions A rigorous thermomechanical model of sedimentary basin evolution comprising a linear elastic-viscoelastic layered lithosphere coupled with both the sediment layer and underlying asthenosphere has been examined. The elastic upper layer in the model is defined by the long-term effective elastic thickness of the lithosphere. The lower warmer part of the lithosphere is relatively weak, and thermomechanical stresses relax there and migrate upwards in a short time compared with the time scale for thermal conduction.