| Project/Area Number |
01302019
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| Research Category |
Grant-in-Aid for Co-operative Research (A)
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| Allocation Type | Single-year Grants |
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| Research Field |
鉱物学(含岩石・鉱床学)
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| Research Institution | Tohoku University |
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Principal Investigator |
AOKI Ken-ichiro (Prof. of Faculty of Sci., Tohoku Univ.), 理学部, 教授 (00004276)
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| Co-Investigator(Kenkyū-buntansha) |
FUJIMAKI Hirokazu (Assoc. Prof. of Faculty of Sci., Tohoku Univ.), 理学部, 助教授 (90133933)
ISHIKAWA Ken-ichi (Assist. of Junior College, Tohoku Univ.), 教養部, 助手 (20158744)
HASENAKA Toshiaki (Assist. of Faculty of Sci., Tohoku Univ.), 理学部, 助手 (50202429)
YOSHIDA Takeyoshi (Assoc. Prof. of Junior College, Tohoku Univ.), 教養部, 助教授 (80004505)
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| Project Period (FY) |
1989 – 1991
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| Project Status |
Completed (Fiscal Year 1991)
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| Budget Amount *help |
¥7,000,000 (Direct Cost: ¥7,000,000)
Fiscal Year 1991: ¥1,500,000 (Direct Cost: ¥1,500,000)
Fiscal Year 1990: ¥1,800,000 (Direct Cost: ¥1,800,000)
Fiscal Year 1989: ¥3,700,000 (Direct Cost: ¥3,700,000)
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| Keywords | upper mantle / basalt / andesite / incompatible element / normalized pattern / volcanic front / island arc / cumulative rock / ソレアイト系列 / カルクアルカリ系列 / 上部マントル / 下部地殻 / 背弧海盆 / アセノスフェア- / 島弧火山岩 / Sr同位体組成 / Nb負異常 / 第四紀火山 / Sr^<87>@Sr^<86> / マグマ |
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| Research Abstract |
In order to elucidate the geochemical and petrological behavior of incompatible trace elements in the Japanese Quaternary basaltic rocks, and the heterogeneity of the source materials in upper mantle, we have determined major and trace elements and Sr and Nd isotopic ratios of the representative volcanic rocks and their incorporated xenoliths derived from upper mantle and lower crust together with their major elements. The following several important results and conclusions have been clarified.
1. All of the basalts and andesites from the East Japan volcanic zone exhibit the nature of typical island arc volcanic rocks'showing the remarkable positive Ba, K and Sr anomalies and the negative Nb anomaly in the rock/primitive mantle normalized pattern for the incompatible elements. Furthermore, their Sr^<87>/Sr^<86> ratios gradually decrease and Nd^<143>/Nd^<144> ratios increase from the volcanic front to the back arc basin side.
2. Alkali series in Japan Sea side have the range of 0.7035 to 0.7050 for Sr^<87>/Sr^<86> ratios and continental characters for incompatible element normalized pattern without any Ba, K, Nb or Sr anomaly.
3. Normalized patterns and Sr and Nd isotopic ratios of cumulative ultranafic to mafic xenoliths derived from upper mantle and lower crust are similar to those of the island. 9rc basalts, and do not have any continental or oceanic basalt natures. It indicates that the basement or uppermost mantle and lower crust of the Japanese islands are composed of cumulative rocks of the island arc basalts.
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