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• W1946757571 endingPage "258" @default.
• W1946757571 startingPage "243" @default.
• W1946757571 abstract "Abstract Formation and deformation processes of the late Paleogene sedimentary basins related to a strike–slip fault system in southern central Hokkaido are described by a combination of paleomagnetic study and numerical analysis. After correction of the Miocene counter‐clockwise rotation associated with back‐arc opening of the Japan Sea, paleomagnetic declination data obtained from surface outcrops in the Umaoi and Yubari areas show significant easterly deflections. Although complicated differential rotation is anticipated as a result of recent thrust movements, clockwise rotation in the study areas is closely linked with development of the Paleogene Minami‐naganuma Basin as a pull‐apart depression along the north–south fault system. Numerical modeling suggests that 30 km of strike–slip is required to restore the distribution and volume of the Minami‐naganuma Basin. The relative slip rate on the long‐standing fault system is about 10 mm/yr, which corresponds to global‐scale plate motion. It has inevitably caused regional rearrangement of the eastern Eurasian margin. A rotation field simulated by simplified dextral motion using dislocation modeling basically accords with the paleomagnetic data around the pull‐apart basin." @default.
• W1946757571 created "2016-06-24" @default.
• W1946757571 creator A5012350748 @default.
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• W1946757571 date "2010-05-26" @default.
• W1946757571 modified "2023-10-17" @default.
• W1946757571 title "Formation and deformation processes of late Paleogene sedimentary basins in southern central Hokkaido, Japan: Paleomagnetic and numerical modeling approach" @default.
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• W1946757571 doi "https://doi.org/10.1111/j.1440-1738.2009.00698.x" @default.
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