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• W2023162582 abstract "The palaeomagnetism of basic rocks and sulphide ores has been studied in the Kure area, Pontic Ranges, Turkey. Progressive alternating-field demagnetization revealed a characteristic remanent magnetization in all investigated rock types except a dacite. The following virtual geomagnetic poles were obtained:Basalt and quartz diabase (oldest): D = 59°, I = +66°, α95 = 4.8, pole 49°N, 93°E. Diabase: D = 210°, I = −15°, α95 = 15.0, pole 47°N, 167°E. Massive sulphide ores: D = 107°, I = +63°, α95 = 8.7, pole 18°N, 80°E. Peridotite: D = 131°, I = +54°, α95 = 10.9, pole 2°S, 72°E. Amphibolitized diabase (youngest): D = 293°, I = +59°, α95 = 12.6, pole 40°S, 145°E.The longidutinal difference in pole positions between the oldest and the youngest rocks is interpreted as being due to a post-Permian counterclockwise rotation of the studied region in relation to the African continent. In addition, there are indications of local rotational movements within the Kure area." @default.
• W2023162582 created "2016-06-24" @default.
• W2023162582 creator A5044519940 @default.
• W2023162582 date "1982-12-01" @default.
• W2023162582 modified "2023-09-27" @default.
• W2023162582 title "A palaeomagnetic study of some basaltoids and ores from the Pontic Ranges, Northern Turkey: Palaeogeographic implications" @default.
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• W2023162582 doi "https://doi.org/10.1016/0040-1951(82)90192-5" @default.
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