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Tectonic implications of paleomagnetic data from upper Cretaceous sediments in the Oyubari area, central Hokkaido, Japan
Author(s) -
Tamaki Machiko,
Itoh Yasuto
Publication year - 2008
Publication title -
island arc
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.554
H-Index - 58
eISSN - 1440-1738
pISSN - 1038-4871
DOI - 10.1111/j.1440-1738.2008.00617.x
Subject(s) - geology , cretaceous , paleontology , paleomagnetism , cenomanian , apparent polar wander , magnetostratigraphy , tectonics , paleogene , geomagnetic pole , continental margin , foraminifera , earth's magnetic field , oceanography , physics , quantum mechanics , magnetic field , benthic zone
Paleomagnetic studies provide constraints on the geometric configuration of the eastern Eurasian margin on geological time scales. Characteristic remanent magnetization components were isolated from eight sites by progressive demagnetization executed on samples from 25 sites in the Oyubari area, central Hokkaido where the Late Cretaceous Yezo Group is distributed. After tilt‐correction, all sites show normal polarity site‐mean directions, and well‐clustered directions pass a positive fold test and a correlation test. Planktonic foraminifera indicate an age range of Cenomanian to Turonian, and the studied section is correlated to the geomagnetic polarity chron C34n. Reliable formation‐mean directions that have been corrected for post‐depositional shallowing (D = 7.5°, I = 65.9°, α 95 = 6.6°) are characterized by inclination data indicative of no significant latitudinal translation since the Late Cretaceous. Central Hokkaido has, therefore, been situated adjacent to easternmost Mongolia including Sikhote Alin around the present latitude since the Late Cretaceous. Declination data require significant differential rotation between Hokkaido and the eastern Asian margin, which may be indicative of rearrangement of crustal blocks along the continental margin.