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  1. 050 理学部
  2. 10 学術雑誌論文
  3. 10 査読済論文
  1. 0 資料タイプ別
  2. 01 学術雑誌論文

日高変成帯、含輝石Iタイプトーナル岩の成因と原岩の溶融度

http://hdl.handle.net/10191/17801
http://hdl.handle.net/10191/17801
5d6ec8a7-f62b-42d4-aff2-60f98dd465cd
名前 / ファイル ライセンス アクション
ZC_105(8)_536-551.pdf ZC_105(8)_536-551.pdf (2.8 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2012-04-11
タイトル
タイトル 日高変成帯、含輝石Iタイプトーナル岩の成因と原岩の溶融度
タイトル
言語 en
タイトル 日高変成帯、含輝石Iタイプトーナル岩の成因と原岩の溶融度
言語
言語 jpn
キーワード
主題Scheme Other
主題 lower crust
キーワード
主題Scheme Other
主題 granulite
キーワード
主題Scheme Other
主題 I-type granite
キーワード
主題Scheme Other
主題 anatexis
キーワード
主題Scheme Other
主題 MORB
キーワード
主題Scheme Other
主題 Hidaka Metamorphic Belt
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
その他のタイトル
その他のタイトル Genesis of the pyroxene-bearing I-type tonalite and melting degree of the source rock, in the Hidaka Metamorphic Belt, northern Japan
著者 志村, 俊昭

× 志村, 俊昭

WEKO 41522

志村, 俊昭

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著者別名
識別子 41523
識別子Scheme WEKO
姓名 Shimura, Toshiaki
抄録
内容記述タイプ Abstract
内容記述 The Hidaka Metamorphic Belt (HMB) is the low P/T type metamorphic belt and represents to a tilted crustal section. The highest metamorphic P-T condition reaches granulite facies. Syn-metamorphic S- and I-type tonalites are intruded into the crustal layer. Large amount of Pyroxene-bearing S-type tonalites are distributed in the Mt. Esaoman-tottabetsu-dake region, northen part of the HMB. The S-type suite is intruded into the granulite facies metamorphic layers and is believed to have crystallized under lower crustal P-T conditions. In the S-type tonalite suite, pyroxene bearing I-type tonalite bodies are found. The I-type tonalites occur as small bodies within the S-type tonalites. Both boundaries are vauge, but some I-type tonalite bodies show chilled margin. The mineral assemblage of the I-type tonalite is Bt+Hbl+Opx±Cpx±Cum+Pl+Qtz. Petrochemical features indicate that the the I-type tonalite generated from mafic metamorphic rocks (N-MORB composition metabasites). Mass balance calculation and batch partial melting modeling indicate that the melting degree is about 29% and 10-30%, respectively. The I-type tonalite is thought to be generated by crustal anatexis of the mafic metamorphic rocks in the lowermost crust.
抄録
内容記述タイプ Abstract
内容記述 日高変成帯北部のエサオマントッタベツ岳地域において,斜方輝石や単斜輝石を含有するIタイプトーナル岩を見いだした.この岩石は下部地殻性のSタイプトーナル岩体内部の小岩体として産する.この岩石について岩石学的研究を行った.その結果,このIタイプマグマはN-MORB組成の塩基性変成岩類が部分溶融して形成されたことが明らかになった.また,その塩基性変成岩類の溶融度は,主成分元素のマスバランスから29%程度,微量元素のモデル計算から10~30%程度であったと推定される.このIタイプトーナル岩は,日高変成帯の最下部地殻のアナテクシスにより発生したマグマであると考えられる.
書誌情報 地質学雑誌
en : 地質学雑誌

巻 105, 号 8, p. 536-551, 発行日 1999-08
出版者
出版者 日本地質学会
ISSN
収録物識別子タイプ ISSN
収録物識別子 00167630
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00141768
著者版フラグ
値 publisher
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