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中部地方水窪地域の中央構造線沿いの領家変成岩類からのカリ長石の三斜度
https://doi.org/10.14945/00000353
https://doi.org/10.14945/00000353536b476b-7998-448b-9be4-b6edeae5925c
名前 / ファイル | ライセンス | アクション |
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KJ00000102429.pdf (1.7 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2008-01-25 | |||||||
タイトル | ||||||||
タイトル | 中部地方水窪地域の中央構造線沿いの領家変成岩類からのカリ長石の三斜度 | |||||||
言語 | ||||||||
言語 | jpn | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | the Median Tectonic Line | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | K-feldspar porphyroblast mylonite gneiss | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | migmatittic granite | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | K-feldspar obliquity | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | inversion | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | upheaval | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | 3-5 mm size K-feldspar obliquity | |||||||
資源タイプ | ||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
資源タイプ | departmental bulletin paper | |||||||
ID登録 | ||||||||
ID登録 | 10.14945/00000353 | |||||||
ID登録タイプ | JaLC | |||||||
タイトル(別言語) | ||||||||
その他のタイトル | The obliquities of K-feldspars from Ryoke metamorphic rocks along the Median Tectonic Line in the Misakubo area, central Japan | |||||||
著者 |
藤吉, 瞭
× 藤吉, 瞭
WEKO
165
× 山田, 真也× 楠, 賢司 |
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書誌情報 |
静岡大学地球科学研究報告 巻 25, p. 9-17, 発行日 1998-07 |
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出版者 | ||||||||
出版者 | 静岡大学地球科学教室 | |||||||
NDC | ||||||||
主題Scheme | NDC | |||||||
主題 | 458 | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | The Ryoke metamorphic rocks along the Mechan Tectonic Line in the Misakubo area connsist of fine-grained gneisses, migmatitic granites and mylonitic rocks. The fme-grained gneisses are pelitic, psamitic and silicious. The migmatitic granites are leucocratic, and occur as veined or dykelike forms ranging from a few centimeters to several tens of centimeter in the fine-grained gneisses. These rocks were metamorphosed under the moderate to higher temperature part of the amnphibolite facies. The mylonitic rocks are close to the Mechan Tectonic Line and consist of mylonitized finegrained gneisses, K-feldspar porphyroblast mylonite gneisses and mylonitized diorite or quartz diorite. We present the obliquities of 113 K-feldspars from the migmatitic granites and K-feldspar porphyroblast mylonite gneisses. From the obliquities of K-feldspars , two events can be recognized in the metamorphic process : in the first event, monoclinic K-feldspars (types I and II ) were formed by regional metamorphism related to migmatization, and triclinic K-feldspars (types IV and V with mean Δ value of 0.83) formed successively by retrogressive dislocation metamorphism closely related with the formation of the Mechan Tectonic Line. The incompleteness of inversion of K-feldspars in the latter might suggest faster upheaval of the metamorphic rocks in the area in comparison with those in the northeastern part of the Hida metamorphic belt. The obliquity study of K-feldspar grains from the K-feldspar porphyroblast mylonite gneisses shows that different grains within one rock specimen have different obliquities. The detailed investigations of 3-5 mm size K-feldspar for a large single crystal reveal that the inversion of monoclinic to triclinic K-feldspar occurs at random in a single grain unlike the suggestion by TOURET (1967) that in a single grain it takes place systematically from the core towards the periphery of the porphyroblast. | |||||||
ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 03886298 | |||||||
NII論文ID | ||||||||
関連タイプ | isIdenticalTo | |||||||
識別子タイプ | NAID | |||||||
関連識別子 | 110000413383 | |||||||
NII書誌ID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AN00103190 | |||||||
フォーマット | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | application/pdf | |||||||
著者版フラグ | ||||||||
出版タイプ | VoR | |||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |