| Project/Area Number |
12440135
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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 | Shinshu University |
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Principal Investigator |
HARAYAMA Satoru Faculty of Science, Geology Department, Professor, 理学部, 教授 (60293536)
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| Co-Investigator(Kenkyū-buntansha) |
MAKINO Kuniaki Faculty of Science, Geology Department, Associate Professor, 理学部, 助教授 (30242712)
YAMAGUCHI Yoshiaki Faculty of Science, Geology Department, Professor, 理学部, 教授 (50144689)
ITAYA Tetsumaru Okayama Science University, Natural Science Laboratory, Professor, 自然科学研究所, 教授 (60148682)
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| Project Period (FY) |
2000 – 2002
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| Project Status |
Completed (Fiscal Year 2002)
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| Budget Amount *help |
¥15,300,000 (Direct Cost: ¥15,300,000)
Fiscal Year 2002: ¥1,200,000 (Direct Cost: ¥1,200,000)
Fiscal Year 2001: ¥1,400,000 (Direct Cost: ¥1,400,000)
Fiscal Year 2000: ¥12,700,000 (Direct Cost: ¥12,700,000)
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| Keywords | Thermochronology / Paleomagnetism / Cooling model / Granite / Mylonite / K-Ar dating / Hida Mountain Range / Uplifting / 閉鎖温度 |
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| Research Abstract |
Thermochronological paleomagnetic and geological studies have been carried out on the Quaternary Takidani Granodiorite and the Late Pliocene Kurobegawa Granite in order to elucidate their cooling history and the mechanism for emplacement. Major results are as follows.
1. Paleomagnetic directions for both the Takidani Granodiorite and the Kurobegawa Granite could not determine for unstability of remanent magnetization of them.
2. Roof volcanic rocks of the above granitic pluton show reversed polarities of remanent magnetization with east-shifted directions as the result of eastward tilting of eastern-half area of the Hida Mountain Range.
3. Both the granitic pluton show strongly mylonitized texture along the N-S tending reverse faults at their western contact.
4. Systematic bottomward younging of biotite K-Ar ages (1.4 Ma to 1.0 Ma) for the Takidani Granodairite can be explained by the slower start in cooling at deeper level of the pluton. Such a cooling history may be affected by the eastward tilting and uplifting of the eastern-half area of the Hida Mountain Range. Mylonitic displacement took place during the cooling process of the Takidani Pluton about 1.0 Ma.
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