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コバヤシ トモユキ
Kobayashi Tomoyuki
小林 記之 所属 スポーツ健康学部 職種 教授 |
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| 言語種別 | 英語 |
| 発行・発表の年月 | 2011/08 |
| 形態種別 | 研究論文（学術雑誌） |
| 標題 | STOP 4-2 : Garnet-rich gneisses (kinzigites), Ktis Quarry, 1 km NNE of Ktis village Coordinates : N48°55'25.33", E14° 8'24.15". |
| 執筆形態 | 共著 |
| 掲載誌名 | 9th International Eclogite Conference in 2011 field guidebook. GeoLines. |
| 掲載区分 | 国内 |
| 巻・号・頁 | pp.96-99 |
| 著者・共著者 | Svojtka, M., Kobayashi, T. and Hirajima, T. |
| 概要 | The garnet-rich gneisses form a ~15 km long, north-south trending, discontinuous belt having up to 100 m in thickness, which forms part of the Lhenice shear zone (Rajlich et al., 1986). The Lhenice shear zone separates the Blansky les granulite massif to the east from the Prachatice and Kristanov granulite massifs to the west. Rajlich et al. (1986) determined that the Lhenice shear zone experienced amphibolite facies metamorphism similar to that in the Varied and Monotonous Units in Lower Austria, i.e. about 0.5 to 0.9 GPa and 700 to 840 °C (Petrakakis, 1986). Detailed gravity profiles of the Lhenice belt presented by Vrana (1979) and Vrana and Sramek (1999) demonstrated that the Lhenice shear zone is a major N-S striking regional shear zone. |