Analysis of partial melting reactions of pelitic and basic metamorphic rocks of the Hidaka metamorphic belt.
| Project/Area Number |
07640631
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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 |
Petrology/Mineralogy/Science of ore deposit
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| Research Institution | Hirosaki University |
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Principal Investigator |
SHIBA Masatoshi Hirosaki University, Department of Earth and Environmental Sciences, Associate Professor., 理工学部, 助教授 (80125442)
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| Co-Investigator(Kenkyū-buntansha) |
NEMOTO Naoki Hirosaki University, Department of Earth and Environmental Sciences, Assistant., 理工学部, 助手 (20208292)
ONUKI Hitoshi Hirosaki University, Department of Earth and Environmental Sciences, Professor., 理工学部, 教授 (00004317)
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| Project Period (FY) |
1995 – 1997
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| Project Status |
Completed (Fiscal Year 1997)
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| Budget Amount *help |
¥2,100,000 (Direct Cost: ¥2,100,000)
Fiscal Year 1997: ¥200,000 (Direct Cost: ¥200,000)
Fiscal Year 1996: ¥700,000 (Direct Cost: ¥700,000)
Fiscal Year 1995: ¥1,200,000 (Direct Cost: ¥1,200,000)
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| Keywords | Hidaka metamorphic rocks / granulite facies / amphibolite migmatite / N-MORB / leucosome / melanosome / mesosome / isocon method / アイソコン法 / 変成条件 / ブラニュライト相 / 温度-圧力-時間経路 / 泥質変成岩 / 塩基性変成岩 / アナテクシス / 部部融解反応 / 部分融解反応 |
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| Research Abstract |
Following results have been obtained by the three-year research (1995,1996 and 1997) supported by this grant.
1.The Hidaka metamorphic rocks were formed by progressive metamorphism under the conditions of the greenschist facies to the granulite facies. The pressure and temperature conditions are estimated to have been 450ﾟC,0.2 MPa to 900ﾟC,0.5 MPa by means of several kinds of geothermometor and geobarometor. The age of the metamorphism are estimated to have been 56-40 Ma (Eocene) on the basis of data of K-Ar dating.
2.Leucosome of pelitic and basic metamorphic rocks of the Hidaka metamorphic belt is solidified parts of melt formed by partial melting of these rocks. On the other hand, melanosome is residue of partial melting.
3.Partial melting reactions of pelitic rocks of the granulite facies (zoneD and zone E) are as follow :
1.3 biotite + 4.6 K-feldspar + 78.3 plagioclase + H_2O = 100 melt + 3.2 sillimanite + 191 quartz (in zone D),
13.4 biotite + 8.6 plagioclase + 15.6 quartz + 16.9 sillimanite = 100 melt + 13.7 K-feldspar + 10.8 cordierite (in zone E).
4.Partial melting reactions of basic rocks (amphibolite migmatites) of the granulite facies (zone E) calculated by the isocon method are as follow :
0.77 hornblende + 10.00 plagioclase + 0.01 limenite = 0.04 magnetite + 10.98 + melt (in the lower temperature part of zone E),
1.85 hornblende + 10.00 plagioclase + 0.0.ilmenite + 12.54 quartz = 0.01 magnetite + 23.96 melt + clinopyroxene (in the higher temperature part of zone E).
5.Protolith of basic metamorphic rocks is basalt of N-MORB compositions.
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Report
(4 results)
Research Products
(16 results)
