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Rock, John

Barth, T. F. W. (1952) Theoretical petrology A textbook on the origin and the evolution of Rocks. John Wiley Sons, New York, 387 pp. [Pg.615]

Rocke, 2004] A. J. Rocke. John Dalton in Lightman, B. ed. Dictionary of Nineteenth-century British Scientists (Bristol Thoemmes), 2004. [Pg.78]

Vol. 27. Rock and Mineral Analysis. Second Edition. By Wesley M. Johnson and John A. Maxwell... [Pg.443]

Vol. 21 Reilctance Spectroscopy. By Wesley Wm.Wendlandt and Harry G. Hecht Vol. 22 The Analytical Toxicology of Industrial Inorganic Poisons. By the late Morris B. Jacobs Vol. 23 The Formation and Properties of Precipitates. By Alan G.Walton Vol. 24 Kinetics in Analytical Chemistry. By Harry B. Mark, Jr. and Garry A. Rechnitz Vol. 25 Atomic Absorption Spectroscopy. Second Edition. By Morris Slavin Vol. 26 Characterization of Organometallic Compounds (in two parts). Edited by Minoru Tsutsui Vol. 27 Rock and Mineral Analysis. Second Edition. By Wesley M. Johnson and John A. Maxwell Vol. 28 The Analytical Chemistry of Nitrogen and Its Compounds (in two parts). Edited by C. A. Streuli and Philip R.Averell... [Pg.651]

New Brunswick s bedrock geology is well mapped and largely well understood. Because of NB s mineral wealth, a great deal of mineral exploration work has been carried out since the 1950s. The bedrock in NB is also diverse in age. The oldest Precambrian rocks can be found in the Saint John area, whereas some of the younger ones, in the form or Triassic basalts, occupy more than half of the Island of Grand Manan. Most of NB s rocks are of Middle Paleozoic age. The triangle between Moncton, Fredericton, and Bathurst is occupied by a thick sequence of Carboniferous rocks that host... [Pg.186]

Two objects with different spectral properties, i.e., variation in the slope of spectral reflectance curve of two bands, can be separable with the help of ratio images (Lillesand et al. 2007). In this study standard reflectance data of USGS Spectral Library and John Hopkins University spectral library (Available in ENVI) have been used. To enhance the dissimilarity between different rock types in the scene, plots with a higher reflectance were kept in the numerator and plots with low reflectance were kept in the denominator, while taking the band ratios. Using this approach, a ratio of 5/3 was taken for basalt, 7/3 for peridotite, and 4/2 for vegetation. [Pg.486]

Figure 5,20 Pyroxene quadrilateral. Solid lines compositionally continuous series dashed tie lines connect compositional terms coexisting on opposite sides of miscibility gap. From G. M. Brown (1967). Mineralogy of basaltic rocks, in Basalts, H. H. Hess and A. Poldervaart, eds., copyright 1967 by John Wiley and Sons. Reproduced with modifications by permission of John Wiley Sons. Figure 5,20 Pyroxene quadrilateral. Solid lines compositionally continuous series dashed tie lines connect compositional terms coexisting on opposite sides of miscibility gap. From G. M. Brown (1967). Mineralogy of basaltic rocks, in Basalts, H. H. Hess and A. Poldervaart, eds., copyright 1967 by John Wiley and Sons. Reproduced with modifications by permission of John Wiley Sons.
Figure 11,17 Whole rock K-Ar isochron of Tuff IB strata from Olduvai Gorge, Tanzania. From G. Faure (1986), Principles of Isotope Geology, 2nd edition, copyright 1986 by John Wiley and Sons. Reprinted by permission of John Wiley Sons. Figure 11,17 Whole rock K-Ar isochron of Tuff IB strata from Olduvai Gorge, Tanzania. From G. Faure (1986), Principles of Isotope Geology, 2nd edition, copyright 1986 by John Wiley and Sons. Reprinted by permission of John Wiley Sons.
Akimoto S., Matsui S., and Syono S. (1976). High-pressure crystal chemistry of orthosilicates and the formation of the mantle transition zone. In The Physics and Chemistry of Minerals and Rocks, R. I G. Strens, ed. New York John Wiley. [Pg.817]

Brown G. M. (1967). Mineralogy of basaltic rocks. In Basalts, H. H. Hess and A. Poldervaart, eds.. New York John Wiley. [Pg.822]

Analyses selected from Table 38 in Deer, W. A., R. A. Howie, and J. Zussman (1963). Rock-Forming Minerals, Vol. 2, pp. 251-253. John Wiley Sons, New York. [Pg.26]

We gratefully acknowledge the financial support for the conference provided by the following Arkansas organizations and individuals Arkansas Electric Power Company Arkansas Louisiana Gas Company BEI Electronics, Inc. First Commercial National Bank General Dynamics Corporation John L. McClellan Memorial Veterans Administration Medical Center Union National Bank University of Arkansas for Medical Sciences Whit Stevens and Winthrop Rockefeller Foundation. Support for publication of this book was provided in part by the Citadel Research Foundation, Little Rock, Arkansas. [Pg.1]

Karl D. Straub John L. McClellan Memorial Veterans Hospital 4300 West 7th Street Little Rock, AR 72205... [Pg.1]

Duke JM. 1980a. Nickel in rocks and ores. In Nriagu JO, ed. Nickel in the environment. New York, NY John Wiley and Sons, Inc., 27-50. [Pg.230]

Engines to Dissipative Structures, John Wiley and Sons, Chichester, UK, 1998 P. A. Rock, Chemical Thermodynamics, University Science Books, Mill Valley, California, 1983 I. M. Klotz and R. M. Rosenberg, Chemical Thermodynamics, Basic Theory and Methods, W. A. Benjamin, Menlo Park, California, 1972. [Pg.42]


See other pages where Rock, John is mentioned: [Pg.79]    [Pg.79]    [Pg.219]    [Pg.191]    [Pg.248]    [Pg.434]    [Pg.17]    [Pg.383]    [Pg.48]    [Pg.409]    [Pg.826]    [Pg.9]    [Pg.189]    [Pg.111]    [Pg.310]    [Pg.7]    [Pg.305]    [Pg.188]    [Pg.13]    [Pg.208]    [Pg.219]    [Pg.1055]    [Pg.86]    [Pg.162]    [Pg.1499]   
See also in sourсe #XX -- [ Pg.208 ]

See also in sourсe #XX -- [ Pg.210 , Pg.546 ]




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