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Geophysical

Given the costs of exploration ventures it is clear that much effort will be expended to avoid failure. A variety of disciplines are drawn in such as geology, geophysics. [Pg.14]

Manghnani M H and Yagi T (eds) 1998 Properties of Earth and Pianetary Maferfa/s (Washington, DC American Geophysical Union)... [Pg.1967]

Submitting the main topic, we deal with models of solids with cracks. These models of mechanics and geophysics describe the stationary and quasi-stationary deformation of elastic and inelastic solid bodies having cracks and cuts. The corresponding mathematical models are reduced to boundary value problems for domains with singular boundaries. We shall use, if it is possible, a variational formulation of the problems to apply methods of convex analysis. It is of importance to note the significance of restrictions stated a priori at the crack surfaces. We assume that nonpenetration conditions of inequality type at the crack surfaces are fulfilled, which improves the accuracy of these models for contact problems. We also include the modelling of problems with friction between the crack surfaces. [Pg.1]

M. A. Meylan, B. K. Dugohnski, and L. Fortin, Bibliography and Index to Eiterature on Manganese Nodules, Key to Geophysical Records documentation No. 6, National Oceanic and Atmospheric Administration, Washington, D.C., 1874—1975, p. 365, p. 60 addendum. [Pg.528]

Other excellent summaries describing what is known of the formation processes and geological setting of these deposits have also been assembled (30—32). Listings of nodule compositions for these and other areas have been compiled (33,34). Eor many sites these data are available as computer databases (qv) maintained by the NOAA National Geophysical Data Center in Boulder, Colorado. [Pg.287]

R. L. Lysak, Auroral Plasma Dynamics, American Geophysical Union, Washiagton, D.C., 1993. [Pg.118]

T. N. Irvine, ed.. Chromium Its Physicochemical Behavior and Petrologic Significance, Carnegie Institution of Washington Conference, Geophysical Laboratory, Pergamon Press, Inc., Elmsford, N.Y., 1977. [Pg.130]

Trofimuk United Institute of Geology, Geophysics and Mineralogy SB RAS Koptyug Pr 3, Novosibirsk 630090, Russia,... [Pg.360]

Grady, D.E. (1977), in High-Pressure Research, Applications in Geophysics (edited by S. Akimoto and M.H. Mangnani) Academic Press, New York, pp. 389-438. [Pg.72]

Figure 4.26. Special radiance versus wavelength for CaAljSi Og glass shocked to 48 GPa and 84 GPa. Best-fitting Planck blackbody curves are shown in relation to the radiance data. (After Boslough and Ahrens (1984). the American Geophysical Union.)... Figure 4.26. Special radiance versus wavelength for CaAljSi Og glass shocked to 48 GPa and 84 GPa. Best-fitting Planck blackbody curves are shown in relation to the radiance data. (After Boslough and Ahrens (1984). the American Geophysical Union.)...
Ahrens, T.J., Lyzenga, G.A., and Mitchell, A.C. (1982), Temperatures Induced by Shock Waves in Minerals, in High Pressure Research in Geophysics (edited by Akimoto S. and M.H. Manghnani), Center for Academic Publications, Japan, pp. 579-594. [Pg.110]

Lindhurst Laboratory of Experimental Geophysics, Siesmological Laboratory 252-21, California Institute of Technology, Pasadena,... [Pg.406]

Arya, S. P., "Introduction to Micrometeorology," International Geophysics Series, Vol. 42. Academic Press, Troy, MO, 1988. [Pg.273]

Australia, is the doyen of materials scientists who study the elastic and plastic properties of minerals under hydrostatic pressure and also phase stability under large shear stresses (Paterson 1973). J.-P. Poirier, in Paris, a professor of geophysics, was trained as a metallurgist one of his special skills is the use of analogue materials to help understand the behaviour of inaccessible high-pressure polymorphs, e.g., CaTi03 perovskite to stand in for (Mg, FelSiOi in the earth s mantle (Poirier 1988, Besson el al. 1996). [Pg.130]

Geophysical techniques can be used for many purposes, such as to (1) map hidden hydrogeologic features, (2) map leachate plumes and zones of... [Pg.118]

It is important to understand that any geophysical method which is successful at one site may or may not have the same success at another site. There are many variables associated with all geophysical techniques as presented in Table 6. Someone with the experience to know the limitations of each of the techniques should be consulted prior to developing a large geophysical reconnaissance program. [Pg.119]

Remote sensing, aerial photography, geophysical techniques... [Pg.120]

Borehole logging and mapping, geophysical techniques (limited)... [Pg.120]

Analysis of groundwater samples from observation wells, geophysics... [Pg.120]

Table 6. Geophysical Techniques, Their Application and Limitations at Hazardous Waste Sites (Johnson, 1986)... Table 6. Geophysical Techniques, Their Application and Limitations at Hazardous Waste Sites (Johnson, 1986)...
Johnson, W. and P. Johnson. "Pitfalls of Geophysics in Characterizing Underground Hazardous Waste," In Management of Uncontrolled Hazardous Waste Sites Proceedings, Hazardous Materials Control Research Institute, Washington, D C., p. 227-232, 1986. [Pg.129]

Zohdy, A., G. Eaton, and D. Mabey. Application of Surface Geophysics to Groundwater Investigation, Techniques of Water Resource Investigation, Book II Chapter Dl, U.S. Government Printing Office, Washington, D.C., 1974, p.l4. [Pg.130]


See other pages where Geophysical is mentioned: [Pg.4]    [Pg.997]    [Pg.150]    [Pg.481]    [Pg.266]    [Pg.165]    [Pg.2]    [Pg.21]    [Pg.355]    [Pg.357]    [Pg.158]    [Pg.317]    [Pg.55]    [Pg.129]    [Pg.129]    [Pg.130]    [Pg.507]    [Pg.118]    [Pg.118]    [Pg.119]    [Pg.126]   
See also in sourсe #XX -- [ Pg.3 ]




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