Relation with caldera-forming eruption and crustal stress field accompanied by sea level change
Project/Area Number |
21340144
|
Research Category |
Grant-in-Aid for Scientific Research (B)
|
Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Geology
|
Research Institution | Fukushima University |
Principal Investigator |
|
Co-Investigator(Renkei-kenkyūsha) |
IKEHARA Ken 産業技術総合研究所, 地質情報研究部門, 研究グループ長 (40356423)
|
Project Period (FY) |
2009 – 2011
|
Project Status |
Completed (Fiscal Year 2011)
|
Budget Amount *help |
¥17,940,000 (Direct Cost: ¥13,800,000、Indirect Cost: ¥4,140,000)
Fiscal Year 2011: ¥650,000 (Direct Cost: ¥500,000、Indirect Cost: ¥150,000)
Fiscal Year 2010: ¥520,000 (Direct Cost: ¥400,000、Indirect Cost: ¥120,000)
Fiscal Year 2009: ¥16,770,000 (Direct Cost: ¥12,900,000、Indirect Cost: ¥3,870,000)
|
Keywords | テフラ / カルデラ形成噴火 / 層序学 / テクトニクス / 海水準変動 / 地質学 / 火山 / 地球変動予測 |
Research Abstract |
In this study, we systematically revealed petrological characteristic such as major elements composition of volcanic glass shard, pyroxene and hornblende which included in Plio-Pleistocene large-scale pyroclastic flow deposits in the Kyushu Island and Miocene to Pleistocene tephra beds in sediment cores drilled at the Nankai Trough. Based on stratigraphical and chronological study, it is possible to evaluate frequency of caldera-forming eruptions in the Kyushu Island and silicic marine explosive eruptions at Izu-Bonin Arc.
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Report
(4 results)
Research Products
(31 results)