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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 38 (1990), S. 0 
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: Total field anomalies as defined from normal aeromagnetic surveys give good approximations of the anomalous components along the direction of the main geomagnetic field, which is generally much larger than the anomalous field. Using the relations between vertical and horizontal components of the field, the total field anomaly is related to any vertical or horizontal component and the corresponding horizontal and vertical derivatives. An example from the Siljan impact structure indicates that such directional filters may be applied to extract useful information from magnetic maps.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 99 (1989), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: In conjunction with airgun profiles on Lake Vänern, 48-channel seismic recordings were made along a 7 km long profile on the northern peninsula, Värmlandsnäs. This peninsula lies in the Mylonite Zone which runs through SW Sweden. Four airgun profiles were recorded, two on the eastern side of the Mylonite Zone and two on the western side, each profile being on the order of 20-30 km long. These profiles have been processed using the method of common data point (CDP) stacking which resulted in a total of approximately 50 km of sub-surface coverage. We have interpreted the data in the context of the regional geology and results from other geophysical studies in the area. Important results are the imaging of lower crustal reflectors and Moho at near-vertical incidence angles. The dips and depths of these reflectors are in fair agreement with other studies. The upper crust on the eastern side of the Mylonite Zone appears to be considerably more reflective. This may be due to the presence of mafic intrusions or to the reworking of the crust during the Sveconorwegian orogeny. A brief comparison with results from the GLIMPCE profiles over the Grenville province is also made.
    Type of Medium: Electronic Resource
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