Study of a Crater Structure found in the south of Takamatsu City, Kagawa Prefecture, Japan Professor
| Project/Area Number |
04452063
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| Research Category |
Grant-in-Aid for General Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Research Field |
固体地球物理学
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| Research Institution | Kanazawa University |
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Principal Investigator |
KONO Yoshiteru Kanazawa Univ., Faculty of Science, Dept. Earth Sciences, 理学部, 教授 (80019489)
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| Co-Investigator(Kenkyū-buntansha) |
YAMADA Isao Nagoya Univ., Faculty of Science, Dept. Earth Sciences, 理学部, 助教授 (60022670)
NAGAO Toshiyasu Kanazawa Univ., Faculty of Science, Dept. Earth Sciences Research Associate Prof, 自然科学研究科, 助手 (20183890)
FURUMOTO Muneyoshi Kanazawa Univ., Faculty of Science, Dept. Earth Sciences Associate, 理学部, 助教授 (80109264)
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| Project Period (FY) |
1992 – 1994
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| Project Status |
Completed (Fiscal Year 1994)
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| Budget Amount *help |
¥7,700,000 (Direct Cost: ¥7,700,000)
Fiscal Year 1994: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 1993: ¥1,800,000 (Direct Cost: ¥1,800,000)
Fiscal Year 1992: ¥5,400,000 (Direct Cost: ¥5,400,000)
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| Keywords | impact crater / gravity anomaly / Takamatsu crater / geomagnetic anomaly / caldera / crater structure / 反射法地震探査 / 地下構造 / ブーゲ異常 / 隕石孔 / カルデラ / 高松市南部 / 磁気異常 / カルデラ孔 |
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| Research Abstract |
A crater-like structure was found in the south of Takamatsu city, Kagawa prefecture, western Japan. This may be the first finding of an impact crater in Japan.
The structure was firstly detected by a abnormal value of gravity which is obtained in a course of regional gravity measurements over the Japanese Islands by us. After several tens of gravity measurements around the anomalous data point, depression of gravity anomaly appeared clearly. This crater was named as the Takamatsu crater. Topography around the crater is nearly flat and no geographical manifestation to indicate a crater-like structure beneath the earth's surface.
More than 500 gravity measurements, geomagnetic anomaly measurements at more than 100 points and 2 sections of reflecting seismic wave measurements were carried out over and around the crater.
Gravity and seismological analysis revealed that the crater is 4 km in diameter and 1.5 km in depth. The structure presumably buried by about 100 m thick Quaternary sediments.
There are two hypothesis about origin of the Takamatsu crater. One is meteorite impact origin, i.e., impact crater. The other is volcanic eruption origin, i.e., caldera.
Already some characteristic minerals are found from the crater area suggesting meteoritic impact origin.
This crater also contains great amount of underground water. Since the crater has not only scientific values but also economical values, we hope that deep drillings undertaken in this crater.
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Report
(4 results)
Research Products
(5 results)
