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- W2012602906 abstract "The present study focuses on some of the Tertiary granitoids of the Rhodope Massif, Northern Greece, namely the Early Miocene plutons of Symvolon, W. Vrondou and the Oligocene Xanthi pluton. Their low-field anisotropy of magnetic susceptibility (AMS) was studied in a number of stations and was combined with existing paleomagnetic and tectonic data in order to check their mutual consistency and to assess to what extent they can help clarifying the tectonic regime prevailing during emplacement of these granitoids. The bulk susceptibility magnitude is generally high, as well as the mean anisotropy degree which reaches 1.23, pointing to a dominant ferromagnetic control of the magnetic properties. Microscopic observation, isothermal remanent magnetization (IRM), and thermomagnetic analysis reveal that the magnetic mineralogy is controlled mainly by magnetite. The magnetic fabrics are well-defined in the plutons, with the Kmax axes (magnetic lineations) varying from gently to moderate plunges. Paleomagnetic results obtained from the same bodies display clear clockwise rotations for all the plutons, with minor or no tilt during their emplacement. Despite of the age differences, the tectonic and magnetic fabrics have mostly similar directions. The prevailing NE–SW-trending linear fabrics, visible mainly in the Early Miocene plutons are also clearly imprinted magnetically in the Early Oligocene pluton, in which no macroscopic fabric is visible. Finally, a preliminary attempt to correct the paleomagnetic results from the magnetic anisotropy effect showed that only qualitative conclusions can be reached from the AMS data, and that complementary AIRM measurements are required." @default.
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- W2012602906 date "2002-01-01" @default.
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- W2012602906 title "A preliminary AMS study in some tertiary granitoids from Northern Greece: integration of tectonic and paleomagnetic data" @default.
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- W2012602906 doi "https://doi.org/10.1016/s1474-7065(02)00115-8" @default.
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