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  • 1
    Description / Table of Contents: We are poised to embark on a new era of discovery in the study of geomorphology. The discipline has a long and illustrious history, but in recent years an entirely new way of studying landscapes and seascapes has been developed. It involves the use of 3D seismic data. Just as CAT scans allow medical staff to view our anatomy in 3D, seismic data now allows Earth scientists to do what the early geomorphologists could only dream of - view tens and hundreds of square kilometres of the Earth's subsurface in 3D and therefore see for the first time how landscapes have evolved through time. This volume demonstrates how earth scientists are starting to use this relatively new tool to study the dynamic of a range of sedimentary environments.
    Pages: Online-Ressource (VII, 274 Seiten)
    ISBN: 9781862392236
    Language: English
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Analytical chemistry 23 (1951), S. 695-699 
    ISSN: 1520-6882
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Analytical chemistry 28 (1956), S. 1427-1430 
    ISSN: 1520-6882
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    European journal of clinical pharmacology 36 (1989), S. 501-506 
    ISSN: 1432-1041
    Keywords: morphine ; cirrhosis ; drug metabolism ; glucuronidation ; hepatic extraction
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Notes: Summary Using hepatic vein catheterization this study has provided the first direct measurement of morphine hepatic extraction in 8 controls and 8 cirrhotics. The extraction ratio was 0.52 in the control group and was reduced by 25% in the cirrhotics. This reduction is due to impaired enzyme capacity rather than reduced blood flow. The effect of cirrhosis is less than that reported in similar studies of high clearance oxidized drugs and this lends support to the concept that glucuronidation may be relatively spared in cirrhosis. A discrepancy between the systemic clearance and the hepatic clearance provides indirect support for extra-hepatic metabolism of morphine.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 174 (1954), S. 801-801 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] These two samples are believed to consist predominantly of condensed poly cyclic aromatic hydrocarbons and to contain also limited quantities of compounds containing oxygen, nitrogen or sulphur in the ring structure or oxygen in phenolic form. Both have a number average molecular weight of about ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Fresenius' Zeitschrift für analytische Chemie 111 (1937), S. 26-28 
    ISSN: 1618-2650
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 7
    Publication Date: 2013-02-02
    Description: The effect of the vertical to horizontal permeability ratio ( k v / k h ) on many displacement properties is significant, making it an important parameter to estimate for reservoir models. Simple ‘streamline’ models have been developed which relate k v / k h at the reservoir scale to shale geometry, fraction and vertical frequency. A limitation of these models, especially for tidally-influenced reservoirs, is the lack of quantitisative geological inputs. To address this lack of data, detailed shale characteristics were measured, using Lidar point clouds, from four different tidally-influenced reservoir analogues: estuarine point bar (McMurray Formation, Alberta, Canada), tidal sand ridge (Tocito Sandstone, New Mexico), as well as both unconfined and confined tidal bars (Sego Sandstone, Utah). Estuarine point bars have long ( x = 67.8 m) shales that are thick and frequent relative to the other units. Tidal sand ridges have short shales ( x = 8.6 m dip orientation) that are thin and frequent. Confined tidal bars contain shales that are thin, infrequent and anisotropic (x– = 16.3 m dip orientation). Unconfined tidal bars contain nearly equidimensional shales of intermediate length ( x = 18.6 m dip orientation) with moderate thicknesses and vertical frequency. The unique shale character of each unit results in a different distribution of estimated k v / k h values. Estuarine point bars have lower average k v / k h values ( x = 8.2 x 10 –4 ) than any other setting because of the long shales they contain. Tidal sand ridges have short, but frequent shales, which results in moderate k v / k h estimates ( x = .011). Estimates of k v / k h are typically highest in confined tidal bars ( x = .038), which contain anisotropic and infrequent shales. Unconfined tidal bars have moderate lengths and frequency resulting in k v / k h estimates averaging 0.004. The results of this study highlight the link between heterogeneity, reservoir architecture and flow parameters.
    Print ISSN: 1354-0793
    Topics: Chemistry and Pharmacology , Geosciences
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  • 8
    Publication Date: 2014-10-15
    Description: A bstract :  Washover fan deposits are part of a much larger system of highly heterolithic barrier and shoreline-margin deposits which form notoriously hard to produce hydrocarbon reservoirs. This survey of modern fan morphologies identifies common fan geometries, considers the preservation potential and range of probable geometries of fan facies in subsurface datasets and outcrops, and aims to improve hydrocarbon recovery in barrier-island reservoir systems. We use satellite imagery to conduct a spatial analysis of 118 modern fans to quantify attributes of fans, including throat width, intrusion length, fan area, and barrier-island width. A new classification scheme for fans is proposed that refines the current fan model. In this classification, fans are initially divided into channelized and non-channelized fans. Channelized fans are subdivided according to the location of primary deposition: barrier depocenter or lagoonal depocenter. Non-channelized fans are subdivided based on morphology: dissipative, lobate, or apron-sourced. Quantitative cross-plots of morphologic parameters are analyzed to define geometric relations in fan morphologies. The probability of identifying fans in the subsurface is discussed. Our results indicate that the most commonly used model for a washover fan, the 52 km 2 St. Joseph Island fan, is anomalous and does not reflect the most common sizes or geometries of washover fans. We suggest that our classification be used instead to capture the range of fan morphologies. Although our study encountered non-channelized, line-sourced, lobate washover fans with an area of less than 1 km 2 more frequently than any other types of fans, washover fans exhibit diverse morphologies; therefore the entire range of washover fan morphologies should be considered when interpreting exploration data and looking to identify washover fans in the subsurface.
    Print ISSN: 1527-1404
    Topics: Geosciences
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  • 9
    Publication Date: 2012-08-01
    Description: A 15,000-km 2 (5792-mi 2 ) three-dimensional seismic data survey that covers the shelf-slope transition of the eastern offshore Trinidad continental margin reveals the geometry and depositional history of the last maximum glacial lowstand shelf-margin succession. Despite the lack of well information at these shallow depths, the quality and continuity of the seismic data allow us to pursue a detailed seismic stratigraphic interpretation of the last lowstand margin succession. The basin-fill stratal architecture of the studied stratigraphic interval shows a great deal of lateral and vertical variability along the continental margin during the Pleistocene to Holocene. Three geomorphological elements controlled the character of the accommodation within the basin and were crucial in transporting, delivering, and storing sediment supply from shelf to slope areas: (1) the Columbus sedimentary pathway on the shelf, (2) bypass zones in the shelf-break region, and (3) deep-water depocenters. The location and geometry of these geomorphological elements within the basin are clearly controlled by underlying structures, transpressional to the north and gravity driven to the south. Migration of the paleo-Orinoco delta system across the shelf was also a key factor in defining the stratigraphic geometries that are observed within the shelf break. Development of shelf-edge versus outer-shelf deltaic systems on the continental margin was controlled by the nature of sediment supply at specific times, as well as by the availability of accommodation, although, to a lesser extent, to relative sea level fluctuations. The interpretation also showed that, for time-equivalent units, parts of the shelf-edge region could develop as an erosional margin (sediment bypass zones), whereas other parts of the shelf edge could behave as an accretionary margin (sediment accumulation). The sequence-stratigraphic interpretation that was attempted in this work also demonstrated that the characteristics of systems tracts can abruptly change along strike in the shelf-edge region for time-equivalent units. These changes can be misleading if a genetic interpretation is pursued only on the basis of the definition of system tracts in the shelf-edge region without the consideration of a complete regional framework.
    Print ISSN: 0149-1423
    Electronic ISSN: 0149-1423
    Topics: Geosciences
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  • 10
    Publication Date: 2013-04-19
    Description: Climate and glacier mass balance trends from 1780 to present within the Columbia Mountains, British Columbia, Canada, were investigated using tree-ring data. Annually resolved ring width, maximum density and maximum cell wall thickness chronologies were constructed from increment core samples of Engelmann spruce ( Picea engelmannii ), mountain hemlock ( Tsuga mertensiana ) and subalpine fir ( Abies lasiocarpa ) trees collected in Glacier and Revelstoke national parks. Proxy records of maximum June–August temperature, August precipitation and February snowpack provide insight into long-term seasonal climate changes. The intervals 1790–1810, 1850–1870 and 1930–1950 were characterized by warm summer temperatures. While overall August precipitation totals decrease over the period of record, the late 1700s, 1805–1835, the 1880s, 1960–1975 and the mid 1980s were notably wetter. February snowpacks have generally decreased in depth since 1873. The reconstructed winter, summer and net mass balance records indicate that glacier cover in the Columbia Mountains has varied primarily in response to decreased snowfall since the mid 1700s. Intervals of terminus advance and retreat were shown to reflect glaciological responses to relatively short-duration variations in summer temperature and winter snowfall. The rate of cumulative mass balance decline within the last 30 years exceeds that observed at any time over the last 250 years.
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
    Published by Sage
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