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  1. B100 理学部/理学研究科
  2. B100d 学位論文
  3. 博士論文(理博・論理博)

Petrology of Pelitic Schists in the Oligoclase-Biotite Zone of the Sanbagawa Metamorphic Terrain,Japan: Phase Equilibria in High-Grade Zone of an Intermediate High-Pressure Metamorphism

http://hdl.handle.net/2237/6384
10e507fd-2137-465a-8b1b-12c731bfbf09
名前 / ファイル ライセンス アクション
ko1608_abstr.pdf ko1608_abstr.pdf (478.8 kB)
ko1608.pdf ko1608.pdf (3.1 MB)
Item type 学位論文 / Thesis or Dissertation(1)
公開日 2006-05-30
タイトル
タイトル Petrology of Pelitic Schists in the Oligoclase-Biotite Zone of the Sanbagawa Metamorphic Terrain,Japan: Phase Equilibria in High-Grade Zone of an Intermediate High-Pressure Metamorphism
その他のタイトル
その他のタイトル 三波川変成帯の灰曹長石-黒雲母帯における泥質片岩の岩石学的研究 -とくに高圧中間群変成作用の高温部における相平衡の解析-
著者 Enami, Masaki

× Enami, Masaki

WEKO 12109

Enami, Masaki

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榎並, 正樹

× 榎並, 正樹

WEKO 12110

榎並, 正樹

Search repository
抄録
内容記述 The oligoclase-biotite zone of the Bessi area, central Shikoku is characterized by sodic plagioclase-bearing assemblages in pelitickl schists, and resents the highest-grade zone of the Sanbagawa metamorphic terrain. Mineral assemblages of pelitic schists in this zone, all with quartz, sodic plagioclase, muscovite and clinozoisite (or zoisite), are garnet + biotite + chlorite + paragonite, garnet + biotite + hornblende +chlorite, and partial assemblages of the above types. Correlations between mineral compositions, mineral assemblages and mineral stability date assuming suggest that metamorphic conditions of this zone are about 610 ± 25°C and 10 ±1Kb. Based upon the comparative study of mineralogy and chemistry of pelitic schists in the oligoclase-biotite zone with those in New Caledonia omphacite zone as a typical high-pressure type and with those in upper staurolite zone as medium-pressure type, progressive as semblages within these zones can be related by such reactions as: omphacite zone garnet + glaucophane + omphacite + muscovite = oligoclase-biotite zone biotite + hornblende + plagioclase + quartz + H2O oligoclase-biotite zone garnet + hornblende + paragonite + muscovite = upper staurolite zone staurolite + biotite + plagioclase + quartz +H2O dP/dT values of these equations calculated using natural compositions are 3-6 and 16-19, respectivel, and their gradients are gentle. This implies that the contrasts of mineral parageneses in pelitic schists related by the aboveequations result mainly from the difference in pressure during progressive metamorphism. A combination of mineral assemblages observed in the Sanbagawa oligoclase-biotite zone represents a characteristic mineral paragenesis of pelitic schists in the high-grade part of an intermediate high-pressure metamorphism.
内容記述タイプ Abstract
内容記述
内容記述 名古屋大学博士学位論文 学位の種類:理学博士 (課程) 学位授与年月日:昭和58年11月4日
内容記述タイプ Other
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_46ec
タイプ thesis
書誌情報 発行日 1983-11-04
学位授与年度
学位授与年度 1983
学位授与年月日
学位授与年月日 1983-11-04
学位授与番号
学位授与番号 13901甲第1608号
フォーマット
application/pdf
フォーマット
application/pdf
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/6384
識別子タイプ HDL
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