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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 123 (1995), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We discuss the results of measurements of the magnetic anomaly field of several seamounts located on the ocean floor and on the bordering continental slopes of the Tyrrhenian Sea. This geomagnetic study of seamounts is based on joint 3-D analyses of the magnetic anomalies and the bathymetry, on measurements of the magnetic properties of rock specimens and on geochronological data. The 3-D analysis of the magnetic anomalies of large volcanoes emplaced in the small oceanic basins of Vavilov and Marsili serves to shed light on the spatial distribution of the magnetized bodies by eliminating the effect of topography. A new magnetic anomaly map of the southern Tyrrhenian Sea is obtained by the merging of shipborne local data, measured on topographic highs, with data of regional type. The study of the magnetic patterns and age of the oceanic seamounts indicates that the volcanic activity mainly developed prior to chron C2 (〉2.02 MaBP) on the Vavilov and Magnaghi edifices (Vavilov Basin), whereas the volcanism of a big oceanic seamount emplaced in the small basin of Marsili took place mainly during the period of chron C1 (0–0.78 Ma BP).
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  Magnetic and gravimetric data from the central Alboran Sea allow identification of two axes of crustal thinning, which were probably active during the Oligocene–Early Miocene. The western Alboran basin axis is subparallel and may be related in origin to the Gibraltar Arc. The ENE–WSW trending Alboran Channel axis is probably intruded by basic igneous rocks and may represent the western end of the Algerian–Balearic basin rift. Present-day small areas with high heat flow may well be related to volcanism and an anomalous mantle. Areas of active deformation in the Alboran Sea accommodate the present Eurasia-Africa convergence.
    Type of Medium: Electronic Resource
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