| Project/Area Number |
05452085
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| Research Category |
Grant-in-Aid for General Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Research Field |
Geology
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| Research Institution | Chiba University |
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Principal Investigator |
TSUKUI Masashi Chiba Univ., Science, Assoc.Professor, 理学部, 助教授 (50192191)
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| Co-Investigator(Kenkyū-buntansha) |
FURUKAWA Noboru Chiba Univ., Science, Res.Associate, 理学部, 助手 (40251194)
HIROI Yoshikuni Chiba Vniv., Science, Professor, 理学部, 教授 (40019427)
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| Project Period (FY) |
1993 – 1995
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| Project Status |
Completed (Fiscal Year 1995)
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| Budget Amount *help |
¥6,900,000 (Direct Cost: ¥6,900,000)
Fiscal Year 1995: ¥800,000 (Direct Cost: ¥800,000)
Fiscal Year 1994: ¥3,400,000 (Direct Cost: ¥3,400,000)
Fiscal Year 1993: ¥2,700,000 (Direct Cost: ¥2,700,000)
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| Keywords | High-grade metamorphics / Partial melting / Garnet / Plagioclase / Compositional zoning / Euhedral outline / Phosphorus minerals / 高温・高圧実験 / 部分溶融実験 / 脱水融解反応 / ミグマタイト / ネオゾーム / ジルコン / 部分溶融 / 高温変成岩 / 泥質岩 / 大陸地殻 / 含水鉱物 / 泥質片麻岩 / 部分溶融(地殻物質の) / 高温高圧実験 / 脱水反応(黒雲母の) |
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| Research Abstract |
The purpose of this study is to establish new indicators of partial melting of high-grade metamorphic rocks which formed at temperatures much higher than those of their minimum melting. First, we looked for textures and compositional features of rock-forming minerals that occur commonly in both igneous and metamorphic rocks, and have found the followings.
1.The common occurrence of euhedral and calcic plagioclase inclusions in garnet porphyroblasts. Inclusion plagioclase is much more calcic compared to the matrix plagioclase.
2.The chemical zoning of garnet and other coexisting cilicate minerals for phosphorus and heavy rare earth elements. Garnet porphyroblasts often consist of phosphorus-poor cores with euhedral and calcic plagioclase inclusions and phosphorus-rich rim with phosphorus mineral inclusions. In addition, garnet often preserves euhedral patterns for heavy rare earth element zonation while major elements zonation patterns are concentric and diffusion controlled. These clearly indicate that phosphorus minerals takes in part of the garnet-forming (partial melting) reaction.
Thus, these features are well explained by the following continuous and incongruent melting reaction :
sillimanite+biotite+sodic plagioclase+quartz+phosphorous minerals<plus-minus>H_2O
=melt+garnet+calcic plagioclase+rutile (or ilmenite)
The amount, morphology, internal structure and compositions of zircon in addition to phosphorus minerals such as apatite, monazite, xenotime and may be significant in geochemical modeling, as shown by the SHRIMP dating.
Part of these features and insights have been reproduced and examined by high-temperature melting experiments with a HIP apparatus.
We also have tried to precisely estimate the temperature, pressure and water content of large-volume felsic magmas erupted from the Aira volcano in Kyushu by experimentally producing phenocryst minerals in them.
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