A Geological and Petrological Study on Plutonic and Metamorphic Rocks in the Southern Abukuma Mountains
| Project/Area Number |
01540649
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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 |
鉱物学(含岩石・鉱床学)
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| Research Institution | Yamagata University |
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Principal Investigator |
TANAKA Hisao Faculty of Science, Yamagata University, 理学部, 助教授 (30007174)
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| Co-Investigator(Kenkyū-buntansha) |
OCHIAI Kiyoshige Science Education Institute of Osaka Prefecture, 研修部, 主任研修員 (00125246)
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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 |
¥2,200,000 (Direct Cost: ¥2,200,000)
Fiscal Year 1991: ¥300,000 (Direct Cost: ¥300,000)
Fiscal Year 1990: ¥400,000 (Direct Cost: ¥400,000)
Fiscal Year 1989: ¥1,500,000 (Direct Cost: ¥1,500,000)
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| Keywords | Abukuma Mountains / Plutonic rocks / Takanuki metamorphic rocks / Tananuka tectonic line / Partial melting / Rare element minerals / S-type / Cataclastic features / 石川岩体 / 角閃岩 / 部分溶融 / 溶融残査 / 鮫川岩体 / 岩石記載 / 変成作用 / 希土類元素規格化パタ-ン / 地質 / 帯磁率 / ミグマタイト / チタン鉄鉱系列 / 鉱物の化学組成 |
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| Research Abstract |
Plutonic and metamorphic rocks in the Abukuma mountains were studied. schistose tonalite, granodioritic rocks and Takanuki metamorphic rocks are distributed in the Samegawa to Hanawa area. These rocks distributing near the Tanakura tectionic line show cataclastic features, such as granulation, elongation and wavy extinction of quartz, bent cleavace and wavy extinction of plagioclase, and kink band and wavy extinction of biotite. The more close to the Tanakura tectionic line, the more intense the cataclastic features are, suggesting that the tectionic line has been active since about 100 ma ago. Partial melting of amphibolite and formation of gabbroic to trondhjemitic veins are observed in the Aakanuki amphibolite in an contact aureole of a dioritic pluton. the host amphibolite is composed of fine grain hornblende + plagioclase (An 70-80) + ilmenite and poor in SiO_2 (-45%), Na_2O and K_2O the veins continuously change their texture, Mineralogy and chemistry from a gabbroic part (SiO_2-45%) to dioritic, and finally to tonalitic or trondhjemitic (SiO_2-70%) Parts.
Granitic rocks in the uzumine area, one of pegmatite-producing spots in the central Abukuma mountains are described. the younger porphyritic two-mica granitic rocks which are considered to be intimately related with pegmatite containing rare element minerals, such as euxenite, monazite and xenotime are the highest in SiO_2 content and exhibit s-type like petrological features.
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Report
(4 results)
Research Products
(13 results)
