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Geophysical exploration

The detection of fresh groundwater is a challenging task in geophysics, because the electrical conductivity of fresh groundwater-bearing aquifers does not differ much from [Pg.410]

Earth field NMR with conventional size coils [Pg.412]

Measurements of longitudinal relaxation would be preferred over measurements of transverse relaxation, because signal attenuation from molecular diffusion in local field gradients near pore walls can then be neglected, but saturation and inversion recovery methods are more time consuming than CPMG experiments, so that transverse relaxation [Pg.413]


Bolt, B. A. (1993). Earthquakes. New York W. II. Freeman. Howell, B. F., Jr. (1990). An Introduction to Seisinological Research. Cambridge, Eng. Cambridge University Press. Kearey, P., and Brooks, M. (1991). An Introduction to Geophysical Exploration. Oxford, Eng. Blaekwell... [Pg.1042]

M.S. Zhdanov and G.V. Keller - The Geoelectrical Methods in Geophysical Exploration... [Pg.249]

Key words Natural gas, Underground storage, Energy reserve, Geophysical exploration, Survey... [Pg.237]

Zhdanov, M. S., and G. Keller, 1994, The geoelectrical methods in geophysical exploration Elsevier, Amsterdam, London, New York, Tokyo, 873 pp. [Pg.28]

In the case of the quasi stationary field, which is the common case in geophysical exploration, we usually ignore the displacement currents (see Chapter 8), which results in a simplification of system (12.1) ... [Pg.362]

M.S. ZHDANOV AND G.V. KELLER —THE GEOELECTRICAL METHODS IN GEOPHYSICAL EXPLORATION... [Pg.613]

Two other pattern-recognition based applications suggest themselves (a) analysis of soil and liquid samples, and (b) geophysical exploration for groundwater. [Pg.71]

Schon J.H., 1996. Physical Properties of Rocks - Fundamentals and Principles of Petrophysics. Handbook of Geophysical Exploration 18, Section I, Seismic Exploration. Pergamon Press, Oxford, 583 pp... [Pg.71]

Abstract The well-known features of the Earth s crust are interpreted as the result of rock fracturing under deep thermodynamic conditions. For this aim, triaxial failure data are scaled up to the crust taking into account temperatures and rock types. The critical depth of hydraulically permeable cracks coincides with the Mohorovicic boundary and that relates to the crust genesis. The annihilation of a crack system at this depth is in accordance with seismic velocity jump known from geophysical exploration. The features of crust floors as well as total thickness, fault inclination, etc, are explained by the suggested mechanical approach. [Pg.727]

Altogether, there were about 164 structures and earthworks identified by the District of Columbia and the Corps of Engineers. However, only 53 POIs have been listed. Except for arsenic, only about a third have been sampled about two-thirds have had any geophysical exploration. Although some of these points encompassed more than one structure, many clearly have been omitted. Only recently has the district received a map locating most of these structures. Indeed, many of these structures have not been located on any map, supporting the author s initial recommendation that the entire 600 acres must be examined. [Pg.128]

Kearey, R, Brooks, M., and Hill, I. 2002. An Introduction to Geophysical Exploration. Blackwell, Oxford. Kramer, F.S., Peterson, R.A., and Walter, W.C. 1968. Seismic Energy Sources—1968 Handbook. Bendix United Geophysical Corporation, Pasadena, CA. [Pg.505]

The shear wave velocity measurement in the field can be carried out either using borings or without borings. Seismic reflection and seismic refraction are staples of conventional geophysical exploration and can provide information on subsurface layer thickness and velocities of propagating waves without need for soil borings. [Pg.22]

A geophysical exploration may be included in a site investigation for an important engineering project in order to provide subsurface information over a large area at reasonable cost. [Pg.346]

The ability to form complex shapes with low-pressure laminates has been utilized in fabricating helium dewars to the optimum shape for specific applications, A typical example is the cryostat assembly of Fig. 6, which is intended for use as an airborne geophysical exploration device.Experience has shown that leakage problems are minimized when a wet layup is used with glass-cloth reinforcement of the epoxy. Attempts to fabricate dewars from preimpregnated tape with an autoclave cure have been less successful, probably because of the many internal joints that provide potential leak paths. [Pg.325]

Aerial geophysical exploration, oil and gas field on a contract basis... [Pg.257]

Bevan, B. W. Roosevelt, A. C. Geophysical Exploration of Guajaia, A Prehistoric Earth Mound in Brazil Geoarchaeology 2003,18,287-331. Young-Sanehez, M. Schaan, D. P. Marajo Ancient Ceramics from the Mouth of the Amazon, Denver Art Museum Denver, CO, 2011. Heckenberger, M. Lost Garden Cities Pre-Colnmbian Life in the Amazon, The Amazon tropical forest is not as wild as it looks. Sci. Am., 2009. http //www.scientificamerican.com/article/lost-cihes-of-the-amazon/ (accessed October 19, 2015). [Pg.86]

Venkatasubramanian, V. S. Studies on radon leakage in minerals. In Geophysical Exploration, A Symposium, Baroda, India, 1959, Proc. New Delhi, Council Sci. Indust. Res., 102—105 (1963). [Pg.129]

Fundamentals Pulsed Methods Continuous Wave Methods Musical Instruments Transducer Arrays Medical Ultrasonics Nondestructive Evaluation Geophysical Exploration Marine Sonar and Sonar In Animals Processing Technology Sonochemistry... [Pg.337]


See other pages where Geophysical exploration is mentioned: [Pg.922]    [Pg.85]    [Pg.416]    [Pg.186]    [Pg.238]    [Pg.319]    [Pg.2]    [Pg.402]    [Pg.410]    [Pg.410]    [Pg.71]    [Pg.506]    [Pg.45]    [Pg.348]    [Pg.325]    [Pg.1773]    [Pg.257]    [Pg.138]    [Pg.1781]    [Pg.118]    [Pg.130]    [Pg.147]    [Pg.353]    [Pg.353]   
See also in sourсe #XX -- [ Pg.410 ]




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