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  • 2005-2009
  • 1990-1994  (3)
  • 1992  (3)
Material
Years
  • 2005-2009
  • 1990-1994  (3)
Year
  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @photogrammetric record 14 (1992), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Notes: A technique for preparing simple, large scale maps of remote and poorly surveyed areas is described, whereby semicontrolled aerial photograph print laydowns are superimposed on enlarged satellite imagery. 〈section xml:id="abs1-2"〉〈title type="main"〉Résumé On décrit une technique permettant de réaliser des cartes à grande échelle, simples, sur des régions lointaines et mal cartographiées: elle consiste à superposer des photomoisai'ques aériennes à des agrandissements ďimages-satellite. 〈section xml:id="abs1-3"〉〈title type="main"〉Zusammenfassung Beschreibung eines Verfahrens zur Herstellung einfacher groβmaβ-stäbiger Karten von entlegenen, nur gering vermessenen Gebieten, wobei paβpunktmäβig gering gestützte Luftbildverbände vergröβerten Satelliten-bildern überlagert werden.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Astrophysics and space science 198 (1992), S. 165-166 
    ISSN: 1572-946X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Fluid source and thermal history are determined for the barite and bitumen-bearing, early Eocene (ca. 50 Ma) polymetallic, epithermal veins of the Owen Lake deposit, central British Columbia, Canada. Carbon isotopic values for the bitumen are highly negative (δ 13 C ca −29%) indicating a probable terrigenous source, which may be 1 no older than Late Cretaceous or, 2 Eocene plant-fossil-bearing units stratigraphically above the Owen Lake deposit. Heat generated by suspected magmatic activity resulted in downflow of meteoric water and upflow of hydrothermal water, mixing at the site of deposition. Aqueous and hydrocarbon fluid inclusions occur within barite; Th of both types of inclusions indicate a temperature range of approximately 100° to 180 °C. Tm(ice) of aqueous inclusions range from −4.5 to −0.2 °C indicating a range of 7.2 to 0.4 equivalent weight percent NaCl. Parageneticaly younger bitumen has a vitrinite reflectance of 0.6% indicating maturation level in the temperature range of 80° to 120 °C, strongly suggesting a cooling thermal regime during barite and bitumen deposition, consistent with a late stage paragenesis.
    Type of Medium: Electronic Resource
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