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- W2130063963 abstract "During the sixth Italian expedition to Victoria Land (Antarctica), Jurassic Ferrar dolerite sills were sampled at 23 sites in the northern Prince Albert Mountains. The rock magnetic properties were similar in all sites. Saturation remanence, remanent coercive force and Curie-temperature values pointed to titanomagnetite as the main carrier of magnetization. Thermal and AF demagnetizations were both effective in removing weak, secondary magnetization components below 250°C and 20 mT peak field. Further demagnetization resulted in single-component, stable ChRM. Palaeomagnetic directions were derived after AF demagnetization at 20 mT, and site-mean VGPs computed for all sites but one (Thern A), where systematic changes of the ChRM inclination have resulted in single-sample VGPs dispersed astride the equator. The site-mean VGPs distribution is clearly bimodal: 15 VGPs cluster around a palaeopole (lat. 48°S, long. 226°E) in good agreement with the literature data, whereas seven VGPs are displaced toward a palaeopole at higher latitude (lat. 79°S, long. 181°E)." @default.
- W2130063963 created "2016-06-24" @default.
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- W2130063963 date "1993-09-01" @default.
- W2130063963 modified "2023-09-29" @default.
- W2130063963 title "Palaeomagnetism of the Ferrar dolerite in the northern Prince Albert Mountains (Victoria Land, Antarctica)" @default.
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- W2130063963 doi "https://doi.org/10.1111/j.1365-246x.1993.tb06983.x" @default.
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