Geomorphic chronology on the marine terraces of the Muroto Peniasula, southwest Japan based on the Milankovitch theory of ice ages.
Project/Area Number |
05452342
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Research Category |
Grant-in-Aid for General Scientific Research (B)
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Allocation Type | Single-year Grants |
Research Field |
自然地理学
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Research Institution | Kobe University |
Principal Investigator |
MATSUSHITA Mariko (1995) Kobe Univ., Research Institude for Higher Education. Technical Official, 大学教育研究センター, 教務職員 (50110804)
田中 眞吾 (1993-1994) 神戸大学, 文学部, 教授 (10031288)
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Co-Investigator(Kenkyū-buntansha) |
KASHIWAYA Kenji Kanazawa Univ., Dep.Earth Science, Assoc.Prof., 理学部, 助教授 (30161029)
TANAKA Shingo Kobe Univ., Emeritus Prof., 名誉教授 (10031288)
松下 まり子 神戸大学, 大学教育センター, 教務職員 (50110804)
野村 亮太郎 神戸大学, 文学部, 助教授 (50164744)
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Project Period (FY) |
1993 – 1995
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Project Status |
Completed (Fiscal Year 1995)
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Budget Amount *help |
¥5,800,000 (Direct Cost: ¥5,800,000)
Fiscal Year 1995: ¥1,300,000 (Direct Cost: ¥1,300,000)
Fiscal Year 1994: ¥1,300,000 (Direct Cost: ¥1,300,000)
Fiscal Year 1993: ¥3,200,000 (Direct Cost: ¥3,200,000)
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Keywords | Milankovitch theory / Marine terrace / Tephra / Pollen analysis / The Muroto Peninsula / 火山灰編年学 / 環境変化 / 物理的性質 / テフラ / 粒度分析 |
Research Abstract |
We have done the geomorphological, tephro-chronological and palynological study on the Marine terraces in the Muroto Peninsula, southwest Japan. and the results are as follow. Field research on marine terraces in the Muroto Peninsula reveals that more than thirty terraces are identified. where formerly only three marin terraces were identified and named H.M and L.The terrace M was considered to have been formed during the last interglacial period, but it becomes clear that the terrace was formed during older interglacial period. The terraces are related to the sea level fluctuation. Each terrace seems to reflect the 20 ky period fluctuation. which is concerned with the precessional parameter of orbit cycle from the Milankovitch theory.
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Report
(4 results)
Research Products
(18 results)