| Project/Area Number |
05835014
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| Research Category |
Grant-in-Aid for General Scientific Research (C)
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| Allocation Type | Single-year Grants |
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| Research Field |
文化財科学
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| Research Institution | OHTANI WOMEN'S UNIVERSITY |
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Principal Investigator |
NAKAMURA Hiroshi OHOTANI WOMEN'S UNIVERSITY PROFESSOR OF LITERAY DEPARTMENT, 文学部, 教授 (10121873)
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| Co-Investigator(Kenkyū-buntansha) |
NAKAJIMA Tadashi FUKUI UNIVERSITY PROFESSOR OF EDUCATIONAL DEPARTMENT, 教育学部, 教授 (70093440)
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| Project Period (FY) |
1993 – 1994
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| Project Status |
Completed (Fiscal Year 1994)
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| Budget Amount *help |
¥1,800,000 (Direct Cost: ¥1,800,000)
Fiscal Year 1994: ¥400,000 (Direct Cost: ¥400,000)
Fiscal Year 1993: ¥1,400,000 (Direct Cost: ¥1,400,000)
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| Keywords | Archaeo-magnetic research / Westan Japan / Chronorogical data / Usikubi-Kiln / Archaeo-magnetic data |
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| Research Abstract |
Our research reaccessed the archaeo-magnetic research data of the objects of ancient Japan found in Westen Japan.The research became more meaningful by combining the traditional chronological data with the archaeo-magnetic data
The way and condition in which the archaeo-magnetic data made pablic were obtained was also reahalized.These data were collected, sorted, and recorded in computer disks.
Also, the data of the Sue ware found together with the objects were reexamined from the archaeo-logical point of view.Graphics were made for the purpose of compavison of the archaeo-magnetic data and the chronorogical data.
All these research, findings, and calculatioms reexamined the aceuracy of age-assumpition of ancient ojujects in the past.Our research foundo that magnetic samphles obtained sometimes were not eventy taken, and, that the samples of remaining burut clay were not taken from the same layr.Our fondings presented the importance and need of more accarate analyzes of the relation between the sample clay and the result of the calculation.
We also made use of the data obtained from the Usikubi-Kiln in Ohnojyo-shi, Fukuoka.Our research found several inportant discrepancies in the archaeo-magnetic data from Kyusyu and Kinki, which had previously been considered being sinilar.
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