| Project/Area Number |
09640509
|
|---|
| Research Category |
Grant-in-Aid for Scientific Research (C)
|
| Allocation Type | Single-year Grants |
|---|
| Section | 一般 |
|---|
| Research Field |
固体地球物理学
|
|---|
| Research Institution | Kagoshima University |
|---|
Principal Investigator |
MIYAMACHI Hiroki Kagoshima University, Faculty of Science, Associate Professor, 理学部, 助教授 (30182041)
|
|---|
| Co-Investigator(Kenkyū-buntansha) |
KOBAYASHI Tetsuo Kagoshima University, Faculty of Science, Associate Professor, 理学部, 助教授 (70112430)
|
|---|
| Project Period (FY) |
1997 – 1998
|
| Project Status |
Completed (Fiscal Year 1998)
|
| Budget Amount *help |
¥1,400,000 (Direct Cost: ¥1,400,000)
Fiscal Year 1998: ¥400,000 (Direct Cost: ¥400,000)
Fiscal Year 1997: ¥1,000,000 (Direct Cost: ¥1,000,000)
|
|---|
| Keywords | Sakurajima / gravity / gravity anomaly / satsuma tephra |
|---|
| Research Abstract |
We carried out geological and gravity surveys in Sakurajima Volcano in order to reveal the detailed gravity anomaly distribution and estimate a location of a crater which produced the biggest eruption 11,000 years ago.
In the geological survey, we investigated a distribution of the Satsuma tephra released from the crater, revealed the detailed stratigraphy, a change and characteristic of the eruptions. We also estimate d that the crater may exists in the western part of Sakurajima from a distribution of the base surge and a direction of trees buried in the base surge.
The gravity survey, which was composed of 346 gravity points, showed the detailed gravity anomaly distribution in Sakurajima. In general, the gravity anomaly gradually changed from the positive anomaly (+12mgal) in the southern area to the negative anomaly (-18mgal) in the northern area. It is also revealed that there is an local area with a negative anomaly (-4mgal) in the Taisho lave area in the western part of Sakurajima. This negative anomaly suggested a low density body in the shallow area from results of a simple numerical experiment. Finally we concluded that this negative anomaly would correspond to a location of the crater which produced the Satsuma tephra.
|
