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Hudson, Rock

The Sherridon complex is one of several arc terranes that form the south flank of the Kisseynew Domain (Fig. 1), a metasedimentary terrane that is part of the Paleoproterozoic Trans-Hudson Orogen. The Kisseynew Domain is dominated by Bumtwood Group metasedimentary rocks and flanked by arc terranes, notably the Lynn Lake Belt to the north and the Flin Flon Belt on the southern flank (Fig. 1). [Pg.404]

Early limestone studies utilized whole-rock samples, but later individual components, such as different generations of cements, have been analyzed (Hudson 1977 Dickson and Coleman 1980 Moldovanyi and Lohmann 1984 Given and Lohmann 1985 Dickson et al. 1990). These studies suggest that early cements ex-... [Pg.202]

Most other developed countries of the world have laws and procedures which direct drug development. Some are not as stringent as those of the United States. This is why you may have seen newspaper accounts of celebrities like Rock Hudson traveling to France for AIDS treatment. There is a current tendency for some medications to be more easily adopted in the United States if they have a history of use in other countries as, for example, with RU-486 (of course, controversy didn t help its case). [Pg.9]

Figure 4 Sulfur isotope summary for black shales from the Pierre Shale of the Cretaceous Western Interior, North America (Gautier, 1986, 1987), and the Jurassic Posidonienschiefer and Jet Rock (Raiswell et al., 1993). For comparison, the maximum fractionation observed in the Posidonienschiefer by Fisher and Hudson (1987) is also shown. The isotopically uniform and strongly S-depleted pyrites of the Jurassic shales and the Cretaceous Sharon Springs Member of the Pierre Shale—like the sediments of the modern Black Sea and Cariaco Basin (Figure 7)—are diagnostic of euxinic (water-column) pyrite formation (see Section 7.06.3.4.2). By contrast, the Cretaceous Gammon Shale shows the S enrichments and broad range of 6 S values possible under oxic depositional conditions (Gautier, 1986, 1987). Figure 4 Sulfur isotope summary for black shales from the Pierre Shale of the Cretaceous Western Interior, North America (Gautier, 1986, 1987), and the Jurassic Posidonienschiefer and Jet Rock (Raiswell et al., 1993). For comparison, the maximum fractionation observed in the Posidonienschiefer by Fisher and Hudson (1987) is also shown. The isotopically uniform and strongly S-depleted pyrites of the Jurassic shales and the Cretaceous Sharon Springs Member of the Pierre Shale—like the sediments of the modern Black Sea and Cariaco Basin (Figure 7)—are diagnostic of euxinic (water-column) pyrite formation (see Section 7.06.3.4.2). By contrast, the Cretaceous Gammon Shale shows the S enrichments and broad range of 6 S values possible under oxic depositional conditions (Gautier, 1986, 1987).
Fisher I. J. St. and Hudson J. D. (1987) Pyrite formation in Jurassic shales of contrasting biofacies. In Marine Petroleum Source Rocks. Geological Society of London Special Pubhcations 26 (eds. J. Brooks and A. J. Fleet). Geological Society of London, London, pp. 69-78. [Pg.3615]

Wastes from lead-rich mineral deposits typically form anglesite in sulfate-dominant environments, but in limestone-dominated host rocks and in gangue containing abundant carbonates, both cerussite [PbCOs] and hydrocerussite [Pb3(-003)2(01-1)2] have been reported as secondary minerals in mining-related wastes. Several carbonate and hydroxycarbonate minerals of copper and zinc were reported by Hudson-Edwards et al. (1996) as secondary products in stream sediments in the Tyne Basin, England. [Pg.4713]

Teresa J. Hudson / Veterans Affairs Medical Center, North Little Rock, Arkansas, U.S.A.,... [Pg.945]

This region is located in the Canadian Shield, composed of massive Precambrian crystalline rocks, mainly granite-gneisses and granites. In the syncline of Hudson Bay, on the south shore, and on the lowlands of the River Mackenzie, there occur sedimentary deposits of Silurian and Devonian dolomites, limestones and sandstones. [Pg.321]

The journey that Arthur Hamilton, 55-year-old banker, will take is to be transformed into a 35-year-old artist, Tony Wilson (Rock Hudson), living in Malibu. Much effort is put into acclimatizing Arthur/Tony to his new life. [Pg.195]

Harrison J. P. and Hudson, J. A. 20(X). Engineering Rock Mechanics Part 2. Illustrative examples, Pergamon, Elsevier Science Ltd., The Boulevard, Longford Lane, Kidlington, Oxford 0X5 I GB, UK. [Pg.286]

Hudson J. A. 1992. Rock engineering systems theory and practice. Ellis Horwood Ltd., Chichester, UK. [Pg.364]

Hudson J. A. (ed.). 2002. Strategy for a rock mechanics site descriptive model. A test case based on data from the Aspo HRL. SKB R-02-... [Pg.364]

If we consider that there are individual binary interactions between these six aspects, there are (6x6 - 6) = 30 separate interactions. The concept of such interactions and the use of an interaction matrix within rock engineering systems have been discussed by Hudson (1992) and the structuring of the features, events and processes related to radioactive waste disposal within an interaction matrix has been used by SKB in Sweden (SKB, 1999). [Pg.434]

Harrison, J.P. Hudson, J.A., 2000. Engineering Rock Mechanics, Part 2 Illustrative Worked Examples, Elsevier, Oxford, U.K. 502p. [Pg.438]

Hudson J. A., 1992. Rock Engineering Systems Theory and Practice. Ellis Horwood, London, 185p. [Pg.438]

Hudson, J. A. Andersson, J., 2003. T-H-M-C modelling of rock mass behaviour 2 - the input data and rock mass partitioning. Proceedings of the GEOPROC2003 conference, Stockholm. [Pg.438]

In Hudson and Harrison (2002), a methodology is proposed for establishing rock mass domains, as shown in Table 1. [Pg.440]

This example, with its generic extrapolation, means that in the numerical modelling consideration must be given to the procedure for dealing with the separate components of the input data. This may involve alternative and sequential rock mass domain partitioning, as described in Hudson and Harrison (2002). [Pg.441]

The approach to the Rock Mechanics Site Descriptive Model was tested by predicting the rock mechanics properties of a 600 m x 180 m x 120 m rock volume at the Aspb Hard Rock Laboratory (HRL) in Sweden using limited borehole data of the type typically obtained during a site investigation (Hudson, 2002). These predicted properties were then compared with best estimate properties obtained from a study of the test rock volume using additional tunnel and tunnel borehole data. This exercise was known as the Test Case, and directly indicates how some of the input required for modelling can be specified and tested. [Pg.443]

Hudson J A Harrison J P, 2002. The principles of partitioning rock masses into structural domains for modeling and engineering purposes. In Mining and Tunnelling Innovation and Opportunity. Proc. of the NARMS-TAC2002 Symposium, Eds. Hammah R., Bawden W., Curran J., Telesnicki M. Univ. Toronto Press, 623-628. [Pg.444]

Andersson, J., Christiansson, R. Hudson, J.A., 2002b. Site Investigations Strategy for Development of a Rock Mechanics Site Descriptive Model. SKB TR 02-01, Swedish... [Pg.444]

Elsworth, D. and Mase, C.R. 1992. Groundwater in rock engineering, Comprehensive rock engineering Principles, practice and projects. Chapters, 1, Hudson, J.A., pp.201-226. [Pg.546]

Ohnishi, Y. Kabayashi, A. 1993. Thermal-hydraulic-mechanical coupling analysis of rock mass. In Hudson J. A. (ed). Comprehensive Rock Engineering, Pergamon Press. 191 - 208... [Pg.758]

Great Work of the alchemists, but it eliminates the prohibitively expensive Precious Metal complex, such as gold and platinum. David Hudson s process extracts the Transition Metals directly from basic and inexpensive sources such as volcanic rock. These are then processed to potable metals, whose primary uses are in medicine and industrial technology. [Pg.14]

Decompression sickness was what afflicted these workers, but they referred to it as the bends. The gigantic pylons that support the bridge had to be constructed deep in the riverbed, and the construction workers labored in large, open-bottomed timber chambers, or caissons, on the floor of the Hudson. Inside these caissons, they toiled away, excavating soil and rock. The surrounding water exerted tremendous pressure on the chamber walls, so the air inside had to be pressurized to prevent the caissons from collapsing. [Pg.15]


See other pages where Hudson, Rock is mentioned: [Pg.307]    [Pg.53]    [Pg.370]    [Pg.307]    [Pg.815]    [Pg.103]    [Pg.419]    [Pg.1338]    [Pg.1341]    [Pg.2480]    [Pg.4712]    [Pg.7]    [Pg.121]    [Pg.474]    [Pg.477]    [Pg.306]    [Pg.360]    [Pg.362]    [Pg.439]    [Pg.842]    [Pg.123]   
See also in sourсe #XX -- [ Pg.7 ]

See also in sourсe #XX -- [ Pg.186 ]




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