| Project/Area Number |
05640527
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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 |
Petrology/Mineralogy/Science of ore deposit
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| Research Institution | Toyama University |
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Principal Investigator |
HORIKOSHI Ei Toyama University Department of Earth Sciences Professor, 理学部, 教授 (30037791)
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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 |
¥2,200,000 (Direct Cost: ¥2,200,000)
Fiscal Year 1994: ¥300,000 (Direct Cost: ¥300,000)
Fiscal Year 1993: ¥1,900,000 (Direct Cost: ¥1,900,000)
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| Keywords | Okhotsk / Sea of Japan / Forearc Volcanism / Miocene / Kitami area / Hornblende / 第三紀花崗岩 / 角閃石安山岩 / 黒鉱 / 根室 / 武佐岳 / 斑晶 |
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| Research Abstract |
It is proposed that the Miocene igneous belts in eastern Hokkaido extends down to the outer zone of Southwest Japan. Igneous rocks, such as 22 Ma-dacitic volcanic conglomerate in Holes 438 and 439, DSDP,and as a heat source for Jyouban hot spring, may connect both Miocene igneous belts. On the contrary the Miocene NE volcanic belt passes through the Oshima Peninsula and attains to the Sea of Japan. There was the zonal arrangement of middle Miocene to Pliocene igneous belts along the Japanese islands from the inner (back-arc) side to outer (trench) one : the arc, monogenic and forearc volcanic belts. The trench during this period was located less than about 100 km far from the forearc volcanic belt.
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