| Project/Area Number |
20540462
|
|---|
| Research Category |
Grant-in-Aid for Scientific Research (C)
|
| Allocation Type | Single-year Grants |
|---|
| Section | 一般 |
|---|
| Research Field |
Petrology/Mineralogy/Science of ore deposit
|
|---|
| Research Institution | Chiba University |
|---|
Principal Investigator |
HIROI Yoshikuni Chiba University, 大学院・理学研究科, 教授 (40019427)
|
|---|
| Co-Investigator(Renkei-kenkyūsha) |
FURUKAWA Noboru 千葉大学, 大学院・理学研究科, 助教 (40251194)
|
|---|
| Research Collaborator |
HOKADA Tomokazu 国立極地研究所, 准教授 (60370095)
SATISH Kumar 静岡大学, 理学部, 准教授 (50313929)
|
|---|
| Project Period (FY) |
2008 – 2010
|
| Project Status |
Completed (Fiscal Year 2010)
|
| Budget Amount *help |
¥4,420,000 (Direct Cost: ¥3,400,000、Indirect Cost: ¥1,020,000)
Fiscal Year 2010: ¥1,170,000 (Direct Cost: ¥900,000、Indirect Cost: ¥270,000)
Fiscal Year 2009: ¥1,170,000 (Direct Cost: ¥900,000、Indirect Cost: ¥270,000)
Fiscal Year 2008: ¥2,080,000 (Direct Cost: ¥1,600,000、Indirect Cost: ¥480,000)
|
|---|
| Keywords | 造山帯 / 下部地殻 / グラニュライト / 岩石の部分融解 / 流体 / 石墨 / 渦巻成長 / 残晶状藍晶石 / 後退的紅柱石 / 部分融解 / 渦巻き成長 / コンダライト / 不純大理石 / スカルン / 累帯構造 / 渦巻き成長模様 / グラニュライト相 |
|---|
| Research Abstract |
The occurrence of various rock types in the deep crust of continental collision zones show definite mutual interactions during partial melting, as revealed by the case study of high-temperature metamorphic rocks occurring near the Syowa Station, Antarctica. The "skarns" developed between pelitic rocks and marble are considered to be the products of the reactions among marble and partial melts of pelitic rocks, which were formed by the infiltration of fluid from the marble. In addition, blocks of Mg-Al-rich granulite containing graphite with spiral growth steps may have experienced partial fusion by the interaction with surrounding marble.
|
