| Project/Area Number |
08454142
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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 |
KAMATA Keiko FACULTY OF SCIENCE,ASSOCIATE PROFESSOR, 理学部, 助教授 (20192544)
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| Co-Investigator(Kenkyū-buntansha) |
MATSUDA Takaaki Dept.Geology, Himeji Inst.Technology, PROFESSOR, 理学部, 教授 (50145827)
INOKUCHI Hiroo Research Center for Inland Seas, KOBE UNIVERSITY,ASSOCIATE PROFESSOR, 助教授 (40112073)
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| Project Period (FY) |
1996 – 1997
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| Project Status |
Completed (Fiscal Year 1997)
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| Budget Amount *help |
¥7,600,000 (Direct Cost: ¥7,600,000)
Fiscal Year 1997: ¥600,000 (Direct Cost: ¥600,000)
Fiscal Year 1996: ¥7,000,000 (Direct Cost: ¥7,000,000)
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| Keywords | remanent magnetization / large-scale pyroclastic-flow deposit / Ata pyroclastic-flow deposit / Ito pyroclastic-flow deposit / annealing temperature / fission-track method / emplacement temperature / アニーリング温度 / 大規模火砕流 / 古地磁気 / 堆積温度 / 溶結 |
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| Research Abstract |
Remanent magnetization and field survey of the Ata large-scale pyroclastic-flow deposit clarified relationship between lithological facies and emplacement temperatures. Palaeomagnetic measurements showed emplacement temperatures of essential fragments and matrix of the pyroclastic-flow deposits higher than 560ﾟC based on the corresponding TRM directions. Three types are identified in the directions of remanent magnetization : (1) single component with the same direction, (2) two components, low and high temperature component, obtained during progressive thermal demagnetization, and (3) components with scattered directions. These results are different from those of the Ito pyroclastic-flow deposit which shows weaker welding than the Ata, suggesting that welding processes start before emplacement.
Reheating process for the Ito pyroclastic-flow deposit was investigated by measuring the annealing temperature of each mineral through track age and length of fission-track method. The anealing temperature of zircon and apatite within granitic fragments in the Ito pyroclastic-flow deposit was estimated to have been between 150ﾟC and 500ﾟC based on the measurement of track length.
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