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ファイル
言語
英語
著者
桜井 剛
柏原 由芙子
南出 幸代
内容記述(抄録等)
A cobble-sized clast of eclogite was recently found in gravels in the bed of the Matsukawa River at Wadano in Hakuba village,Nagano Prefecture.The cobble was probably derived from an area in the Hida Marginal belt,which consists of high-pressure type schists and closely associated serpentinites,and also includes blocks of garnet glaucophane schist and garnet-epidote-glaucophane schist.
The eclogite cobble consists mainly of garnet,omphacite,epidote and amphibole,along with small amounts of quartz,albite,chlorite,phengite,apatite,rutile,titanite and pumpellyite.Amphibole occurs as abmdant subhedral prismatic crystals showing distinct zoning,with bluish cores and greenish rims.The cores of such amphiboles often have resortion texture,and are overgrown by green amphibole at their rims.The boundaries between the cores and rims are sharp and abrupt.The cores ofthe prismatic amphibole are chemically classified as glaucophane,whereas the rims are divided into two parts;inner rims consisting of barroisite,and outer rims of actinolite.
The eclogite described in this paper shows a typical clockwise P-T path of metamorphism,which is composed of a prograde path from the glaucophane schist facies to form eclogite,and a retrograde path from eclogite through the epidote amphibolite to the greenschist facies.
掲載誌名
島根大学地球資源環境学研究報告
22
開始ページ
167
終了ページ
172
ISSN
13439774
発行日
2003-12-27
NCID
AA11455176
出版者
島根大学総合理工学部地球資源環境学教室
出版者別表記
Department of Geoscience, Interdisciplinary Faculty of Science and Engineering, Shimane University
資料タイプ
紀要論文
部局
(旧組織)大学院総合理工学研究科
備考
12-14,16+ / 1993+
飯泉滋教授・山内靖喜教授 退官記念特集号
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