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Author: National Measurement Laboratory (U.S.). Office of Standard Reference Materials
Publisher:
ISBN:
Category : Materials
Languages : en
Pages : 160
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Author: National Measurement Laboratory (U.S.). Office of Standard Reference Materials
Publisher:
ISBN:
Category : Materials
Languages : en
Pages : 160
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Book Description
Author: National Institute of Standards and Technology (U.S.)
Publisher:
ISBN:
Category :
Languages : en
Pages : 452
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Author: United States. National Bureau of Standards
Publisher:
ISBN:
Category :
Languages : en
Pages : 470
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Category : Weights and measures
Languages : en
Pages : 456
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Author: National Measurement Laboratory (U.S.). Office of Standard Reference Materials
Publisher:
ISBN:
Category : Materials
Languages : en
Pages : 112
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Category : Geology
Languages : en
Pages : 84
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Author: Arthur Edward Nelson
Publisher:
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Category : Basalt
Languages : en
Pages : 280
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Deformation Quadrangle, 1n the Stensgar Mountain Stevens County, Washington By James G. Evans Abstract Most deformation of the Middle and Late Proterozoic (Deer Trail and Windermere Groups) and Lower Cambrian (Addy Quartzite and Old Dominion Limestone) rocks in the Stensgar Mountain quadrangle occurred during the Mesozoic (pre-Late Jurassic, possibly Early Jurassic or Triassic), in con- nection with duplex thrusting. The principal deformation occurred in stages that generally involved: (1) thrusting, (2) penetrative dynamothermal metamorphism in the greenschist facies, and (3) renewed thrusting. The initial thrusting may have included formation of the duplex fault zone, moderate tilting of the sedimentary and volcanic rocks, and possibly low-grade metamorphism. The dynamothermal metamorphism resulted in development of a slaty cleavage that dips steeply west, as well as numerous minor and a few large folds that plunge at low to moderate angles, generally north. The folds have axial planes parallel to cleavage. Clasts in conglomerates were flattened parallel to cleavage, and their long axes were aligned north-northeastward, subparallel to fold axes. This extension direction parallels the trend of the Kootenay arc, a relation not typical of orogenic belts. The dynamothermal metamorphism included coaxial compressive pulses separated by periods of stress relaxation. The penetra- tive deformation could have been accompanied by slip on preexisting faults, including a large strike-slip component for the roof (Stensgar Mountain thrust) and floor (Lane Mountain thrust) thrusts of the duplex fault zone. Later movements along these roof and floor thrusts and connecting splays are suggested by nonfolded traces of the faults and the faulted, dynamothermally metamorphosed cataclasite adjacent to the Lane Mountain thrust. The penetrative deformation that affected the Stensgar Mountain quadrangle also affected the rest of northeastern Washington and southeastern British Columbia; it may have been the result of oblique convergence during Mesozoic subduction.
Author: National Measurement Laboratory (U.S.). Office of Standard Reference Materials
Publisher:
ISBN:
Category : Materials
Languages : en
Pages : 96
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Author:
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Category : Government publications
Languages : en
Pages : 570
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Author: Jan Kucera
Publisher: Springer Science & Business Media
ISBN: 1475760256
Category : Science
Languages : en
Pages : 715
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Nuclear Analytical Methods in the Life Sciences •1994 is a forefront survey of key presentations from the 1993 International Conference on Nuclear Analytical Methods in the Life Sciences. Sponsored by the International Atomic Energy Agency (IAEA), this useful volume covers the spectrum of multidisciplinary research on both the methodological aspects and the development of nuclear analytical methods and their applications in the life sciences. The book is divided into six sections covering related material. These sections are: Methodology of Nuclear Analytical Methods; Environmental Applications; Biomedical Applications; Analysis of Biological Samples; Quality Assurance and Comparison with Other Methods; and a section dealing with miscellaneous issues, such as programs offered by the IAEA.
