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Tarantola, A., 1987, Inverse Problem Theory, Elsevier Tarantola, A., Valette, B., 1982, Generalized nonlinear inverse problems solved using the least squares criterion. Reviews of Geophysics and Space Physics 20, 219... [Pg.421]

Izawa et al. (1990) reviewed the studies on the geology, geophysics and geochemistry which had been done during 1980s. [Pg.183]

Stumm, W. and R. Wollast, 1990, Coordination chemistry of weathering, kinetics of the surface-controlled dissolution of oxide minerals. Reviews of Geophysics 28, 53-69. [Pg.531]

Gale, N.H. and Mussett, A.E. (1973). Episodic uranium-lead models and the interpretation of variations in the isotopic composition of lead in rocks. Reviews of Geophysics and Space Physics 11 37-86. [Pg.341]

Mangold DC, Tsang C-F. 1991. A summary of subsurface hydrological and hydrochemical models. Reviews of Geophysics 29 51-79. [Pg.270]

Figure 3J Schematic representation of a vibrational spectrum of a crystalline phase. Dotted curves acoustic branches and optical continuum. Solid line total spectrum, and 0) 2 Einstein oscillators. Reprinted with permission from Kieffer (1979c), Review of Geophysics and Space Physics, 17, 35-39, copyright 1979 by the American Geophysical Union. Figure 3J Schematic representation of a vibrational spectrum of a crystalline phase. Dotted curves acoustic branches and optical continuum. Solid line total spectrum, and 0) 2 Einstein oscillators. Reprinted with permission from Kieffer (1979c), Review of Geophysics and Space Physics, 17, 35-39, copyright 1979 by the American Geophysical Union.
Figure 6AO Temperature dependence of enthalpy (A) and heat capacity (B) for CaMg-Si206 component in crystalline, vitreous, and molten states at various T conditions. Reprinted with permission from Richet and Bottinga (1986), Review of Geophysics and Space Physics, 24, 1-25, copyright 1986 by the American Geophysical Union. Figure 6AO Temperature dependence of enthalpy (A) and heat capacity (B) for CaMg-Si206 component in crystalline, vitreous, and molten states at various T conditions. Reprinted with permission from Richet and Bottinga (1986), Review of Geophysics and Space Physics, 24, 1-25, copyright 1986 by the American Geophysical Union.
Figure 11.29 Specific radioactivity of expressed as per-mil deviation (A%o) from present-day radioactivity over the last 7500 years, derived from comparisons with dendrochronological studies. Reprinted from Damon et al. (1978a), with permission, from The Annual Review of Earth and Planetary Sciences, Volume 6, copyright 1978 by Annual Reviews Inc. and from Suess (1965), Journal of Geophysical Research, 70, 5937-5952, copyright 1965 by the American Geophysical Union. Figure 11.29 Specific radioactivity of expressed as per-mil deviation (A%o) from present-day radioactivity over the last 7500 years, derived from comparisons with dendrochronological studies. Reprinted from Damon et al. (1978a), with permission, from The Annual Review of Earth and Planetary Sciences, Volume 6, copyright 1978 by Annual Reviews Inc. and from Suess (1965), Journal of Geophysical Research, 70, 5937-5952, copyright 1965 by the American Geophysical Union.
Figure 11.30 Reduced partition function for various minerals calulated by Kieffer (1982) through equation 11.61 plotted against T. Heavy curve labeled H20(l) is reduced partition function of water according to Becker (1971). Dashed curve is a extrapolation of high-r reduced partition curve for quartz. Mineral abbreviations Qtz (quartz), Calc (calcite), Albt (albite), Muse (muscovite), Enst (clinoenstatite), Anor (anorthite). Diop (diopside), Pyrp (pyrope), Gros (grossular), Zron (zircon), Fors (forsterite), Andr (andra-dite), Rutl (rutile). Reprinted with permission from Kieffer (1982), Review of Geophysics and Space Physics, 20, 827-849, copyright 1982 by the American Geophysical Union. Figure 11.30 Reduced partition function for various minerals calulated by Kieffer (1982) through equation 11.61 plotted against T. Heavy curve labeled H20(l) is reduced partition function of water according to Becker (1971). Dashed curve is a extrapolation of high-r reduced partition curve for quartz. Mineral abbreviations Qtz (quartz), Calc (calcite), Albt (albite), Muse (muscovite), Enst (clinoenstatite), Anor (anorthite). Diop (diopside), Pyrp (pyrope), Gros (grossular), Zron (zircon), Fors (forsterite), Andr (andra-dite), Rutl (rutile). Reprinted with permission from Kieffer (1982), Review of Geophysics and Space Physics, 20, 827-849, copyright 1982 by the American Geophysical Union.
Kvenvolden, K. A. (1993). Gas hydrates-geological perspective and global change. Reviews in Geophysics, 31(2), 173. [Pg.47]

Mitchell, J. F. B. 1989. The greenhouse effect and climate change, Review of Geophysics, 27, 115-139. [Pg.167]

McSween, H. Y. (1979) Are carbonaceous chondrites primitive or processed A review. Reviews of Geophysics and Space Physics, 17, 1059-1078. [Pg.190]

Scott, E. R. D. and Wasson, J. T. (1975). Classification and properties of iron meteorites. Reviews of Geophysics and Space Physics, 13, 527-546. [Pg.190]

Grossman, L. and Larimer, J. W. (1974) Early chemical history of the solar system. Reviews of Geophysics and Space Physics, 12, 71—101. [Pg.227]

Borg, L. and Drake, M. J. (2005) A review of meteorite evidence for the timing of magmatism and of surface or near-surface liquid water on Mars. Journal of Geophysical Research, 110, E12S03. [Pg.348]

This chapter reviews and clarifies some of the main features in the pattern and rate of transport of nuclear bomb debris from the upper atmosphere down to the surface of the earth. The atmospheric nonmen-clature used is that based on the thermal structure of the atmosphere and recommended by the International Union of Geodesy and Geophysics at Helsinki in 1960, shown in Figure 1. Starting with the lower thermosphere, the important mechanisms of vertical transport are discussed... [Pg.147]

Fig. VIII -11. Observed concentrations of trace species in the stratosphere. From Johnston (543). Data on CCIjF and CCIjFj are from Heidt et al. (460). V/ V is the volume mixing ratio. Reprinted by permission of Annual Reviews, Inc. and the American Geophysical Union. Fig. VIII -11. Observed concentrations of trace species in the stratosphere. From Johnston (543). Data on CCIjF and CCIjFj are from Heidt et al. (460). V/ V is the volume mixing ratio. Reprinted by permission of Annual Reviews, Inc. and the American Geophysical Union.
Rodgers, C. D (1976) Retrieval of Atmospheric Temperature and Composition From Remote Measurements of Thermal Radiation, Reviews of Geophysics and Space Physics, 14,609. [Pg.347]

Wagner, B. J. (1995). Recent advances in simulation-optimization groundwater management modeling P Reviews of Geophysics, Supplement, 1021-1028. [Pg.44]

Smith, S. V., and J. T. Hollibaugh. 1993. Coastal metabolism and the oceanic organic carbon balance. Reviews of Geophysics 31 75-89. [Pg.362]

Khandekar M.L. Murty T.S. and Chittibabu P. (2005). The Global Warming Debate A Review of the State of Science. Pure and Applied Geophysics, 162(8-9), 1557-1586. [Pg.535]


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