2009 Fiscal Year Final Research Report
Thermobaric structure of Himalayan UHP metamorphic belt induced by zircon inclusion method
Project/Area Number |
19540477
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Research Category |
Grant-in-Aid for Scientific Research (C)
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Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Geology
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Research Institution | Meisei University |
Principal Investigator |
KANEKO Yoshiyuki Meisei University, 理工学部, 准教授 (50397080)
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Project Period (FY) |
2007 – 2009
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Keywords | ジルコン / ヒマラヤ / 超高圧変成岩 / 顕微ラマン |
Research Abstract |
Coesite relics were discovered as inclusions in Cpx in eclogite and as inclusions in zircon in felsic and pelitic gneisses from Higher Himalayan Crystalline rocks in upper Kaghan valley, north-west Himalayas. The metamorphic peak conditions of the ultrahigh-pressure (UHP) eclogites are estimated to be 28.6±0.4 kbar and 757-786℃. The Himalayan UHP metamorphic rocks crops out a very thin layer (<100m) sandwiched between overlying and underlying medium to high-pressure metamorphosed units. This imply that the very thin UHP layer moved up from the mantle depth (95-120km) to the mid-crustal level (30-40km), then stopped and thermally altered the surrounding the Higher Himalayan Crystalline rocks.
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[Journal Article] On-going orogeny in the outer-arc of Timor-Tanimber region, eastern Indonesia.2007
Author(s)
Kaneko, Y., Maruyama, S., Kadarsman, A., Ota, T., Ishikawa, M., Tujimori, J., Ishikawa, A., Okamoto, A.
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Journal Title
Gondwana Research. 11
Pages: 218-233
Peer Reviewed
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