Tectonics of eastern margin of the Asian continent
| Project/Area Number |
09440175
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| Research Category |
Grant-in-Aid for Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Geology
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| Research Institution | Kobe University |
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Principal Investigator |
OTOFUJI Yo-ichiro Kobe University, Dept. Science, Professor, 理学部, 教授 (90160895)
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| Co-Investigator(Kenkyū-buntansha) |
MATSUDA Takaaki Himeji Institute of Technology, Dept. Science, Professor, 理学部, 教授 (50145827)
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| Project Period (FY) |
1997 – 1999
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| Project Status |
Completed (Fiscal Year 1999)
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| Budget Amount *help |
¥9,700,000 (Direct Cost: ¥9,700,000)
Fiscal Year 1999: ¥1,200,000 (Direct Cost: ¥1,200,000)
Fiscal Year 1998: ¥1,200,000 (Direct Cost: ¥1,200,000)
Fiscal Year 1997: ¥7,300,000 (Direct Cost: ¥7,300,000)
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| Keywords | PALEOMAGNETISM / CONTINENT / DEFORMATION / TECTONICS / 阿武隈 / 南薩 / 日本列島 / 南部北上 / 宮守苦鉄質岩体 / 濃飛流紋岩 / 東アジア / 白亜紀 / 古第三紀 / 年代学 |
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| Research Abstract |
We carried out our paleomagnetic study in Kitakami massif in Northeast Japan, Nohi area in easternpart of Southwest Japan, and Sikhote Alin mountain in Russia.
Paleogene and early Cretaceous welded tuffs have been sampled from eleven sites at the Omoe Peninsula(39.6°N,142.0°E) in the Kitakami massif of northeast Japan for paleomagnetic study. Westerly declinations with shallow inclination are identified after tilt correction in the 62〜71 Ma Heizaki volcanics(D=283.5°,I=9.4°, αィイD295ィエD2=8.0°) and in the 114〜119 Ma Harachiyama Formation(D=274.2°, I=-20.4°). The shallow inclination indicates that the Kitakami massif was located in low latitude(5°±4°N) at 62〜71 Ma. Taking into account a reference paleomagnetic pole of the Paleocene expected from Sikhote Alin, the Kitakami massif was translated northward over 25° in latitude since 65 Ma. We conclude that the Kitakami massif was incorporated into Asian continent at some time between 30 Ma and 22 Ma before opening of the Japan Sea.
We investig
… More
ate formation of the curvature of the Median Tectonic Line (MTL) in Southwest Japan. we carried out a paleomagnetic study in the Nohi area, north of the curved part of the MTL in the eastern part of Southwest Japan. Paleomagnetic data indicate that the Nohi area are experienced a clockwise rotation through more than 45° with respect to the Asian continent as a part of Southwest Japan but that the amount of rotation of the Nohi area is 23°smaller than that of the central part of Southwest Japan. A new model is developed to explain the tectonic rotation. At about 15 Ma during the latest stage of the clockwise rotation of Southwest Japan associated with opening of the Japan Sea, the eastern end moved southward by more than 60 km along a lest-lateral strike-slip fault which comprised the present north-south segment of the MTL and the Akaishi Tectonic Line. We conclude that the curvature of the MTL is a composite of the 15 Ma strike-slip fault system and a small bend of the MTL associated with the small differential rotation of the Nohi area with respect to the central part of Southwest Japan. Less
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Report
(4 results)
Research Products
(12 results)
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[Publications] Uno,K., Y.Otofuji, T.Matsuda, Y.Kuniko, R,Enami, R.G.Kulinich, P.S.Zimin, A.P.Matunin and V.G.Sakhno: "Late Cretaceous paleomagnetic results from Northeast Asian continental margin : The Sikhote Alin mountain range, eastern Russia"Geophys. Res. Lett.. 26. 553-556 (1999)
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