Study on high- and ultrahigh- temperature metamorphic rocks and partial melting, with a point of view of quartz occurrence
| Project/Area Number |
17540432
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| Research Category |
Grant-in-Aid for Scientific Research (C)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Geology
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| Research Institution | Niigata University |
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Principal Investigator |
SHIMURA Toshiaki Niigata University, Institute of Science and Technology, Associate Professor (70242451)
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| Project Period (FY) |
2005 – 2007
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| Project Status |
Completed (Fiscal Year 2007)
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| Budget Amount *help |
¥3,850,000 (Direct Cost: ¥3,700,000、Indirect Cost: ¥150,000)
Fiscal Year 2007: ¥650,000 (Direct Cost: ¥500,000、Indirect Cost: ¥150,000)
Fiscal Year 2006: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 2005: ¥2,700,000 (Direct Cost: ¥2,700,000)
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| Keywords | quartz / granite / metamorphic rocks / cathodoluminescence / partial melting / Hidaka Metamorphic Belt / granulite / zircon / REE / CHIME / EPMA |
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| Research Abstract |
Psammitic and pelitic rocks are SiO2 saturated rocks. On the partial melting process, quartz occurrence and silica saturation index are the important factors. However, modal composition of quartz is ignored as an excess component for the equilibrium computation. The purpose of this study is, analysis of timing of metamorphism, partial melting, and granitic melt separation, by the cathodoluminescence (CL) image, with a point of view of quartz occurrence.
This project made innovative results. These are, we had found out older stage cores of zircon in the granulite, migmatite, tonalite, are residual material of the sediment. These must be residual grain of sediment. Whereas we also found out that bright rims is the new growth pert by the partial melting. We also revealed the age of the bright rims.
Our results changed the tectonic history of the Hidaka Metamorphic Belt.
These are:
(1) Main thermal event is not 55Ma. That was two times, 37Ma and 19Ma.
(2) 37Ma is island-arc type igneous activity.
(3) 19Ma is another igneous activity related by back-arc basin opening. This stage is the MORB-type activity and the granulite facies high-temperature metamorphism.
Our result was published by "Geology", and also newspapers. The CL detector was indispensable item for the new discovery.
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Report
(4 results)
Research Products
(43 results)
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[Journal Article] Issues relating to Rb-Sr and Sm-Nd whole rock isochrons2007
Author(s)
Kagami, H., Imaoka, T., Ishioka, J., Kagashima, S., Kawano, Y., Osanai, Y., Owada, M., Shimura, T., Shiraishi, K., Yuhara, M
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Journal Title
Description
「研究成果報告書概要(欧文)」より
Related Report
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[Journal Article] Nakano, S., Geological Map of Japan 1:50000, Suhara2005
Author(s)
Takahashi, Y., Toyoshima, T., Shimura, T., Hara, H., Takeuchi, K., Sakai, A. Nakano, S
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Journal Title
Chishitu News 607
Pages: 57-62
Description
「研究成果報告書概要(欧文)」より
Related Report
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[Journal Article] Cooling process of the basal tonalite magma, Hidaka metamorphic belt, northern Japan2005
Author(s)
Shimura, T., Osanai, Y., Toyoshima, T., Owada, M. ,Komatsu, M
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Journal Title
Jour. Geol. Soc. Japan 112
Pages: 654-665
NAID
Description
「研究成果報告書概要(欧文)」より
Related Report
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[Journal Article] Partial melting of high-grade metamorphic rocks in lower crustal part of the Hidaka Arc(Main Zone of the Hidaka metamorphic belt), northern Japan2005
Author(s)
Osanai, Y., Owada, M., Shimura, T., Nakano, N., Kawanami S., Komatsu, M
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Journal Title
Jour. Geol. Soc. Japan 112
Pages: 623-638
NAID
Description
「研究成果報告書概要(欧文)」より
Related Report
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