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The latter part ranging from several milimeters to about one centimeter is scattered in the dominant former part. The two parts are microscopically mixed up irregularly in a micron-order, too. The transparent part is clear, and cryptoperthitic of braid-type or lamellar type, or featureless without microtextute, and the pinkish part is turbid and microperthitic of vein-type under an optical microscope. Both the microperthite and braid-cryptoperthite were examined with EPMA\n, and the size, form and orientation of lamellae or vein, distribution of micropores in both the clear and turbid parts, and compositional variation patterns in microperthitc Ab-rich veins were clrified. The textural features of the alkali feldspar are principally similar to those of the Klokken syenite feldspars. The Klokken model of feldspar cooling, which advocates deuteric coarsening of cryptoperthite to microperthite with micropore formation at the hydrothermal\n stage in plutonic rocks, may be appllicable to the Hanazono alkali feldspar, in spite of the difference of their bulk compositions. Irregular and complicated Ca distribution\n patterns in the Hanazono Ab-rich veins, however, throw new insight to the Klokken cooling model.", "subitem_description_type": "Abstract"}]}, "item_2_description_7": {"attribute_name": "引用", "attribute_value_mlt": [{"subitem_description": "滋賀大学教育学部紀要, 3, 自然科学, 第47号, pp.25-39", "subitem_description_type": "Other"}]}, "item_2_full_name_2": {"attribute_name": "著者(ヨミ)", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "7957", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "ナカノ, サトシ"}]}, {"nameIdentifiers": [{"nameIdentifier": "7958", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "エリグチ, タカユキ"}]}]}, "item_2_full_name_3": {"attribute_name": "著者別名", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "7959", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Nakano, Satoshi"}]}, {"nameIdentifiers": [{"nameIdentifier": "7960", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Eriguchi, Takayuki"}]}]}, "item_2_publisher_35": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "滋賀大学教育学部"}]}, "item_2_source_id_11": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AA11123267", "subitem_source_identifier_type": "NCID"}]}, "item_2_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1342-9272", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "中野, 聰志"}], "nameIdentifiers": [{"nameIdentifier": "7955", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "江里口, 隆之"}], "nameIdentifiers": [{"nameIdentifier": "7956", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2018-09-12"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "SJ10_0047_025A.pdf", "filesize": [{"value": "20.8 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 20800000.0, "url": {"label": "SJ10_0047_025A.pdf", "url": "https://shiga-u.repo.nii.ac.jp/record/1707/files/SJ10_0047_025A.pdf"}, "version_id": "57459a9b-8705-4643-bb6f-fb7d03272015"}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "jpn"}]}, "item_resource_type": {"attribute_name": "資源タイプ", "attribute_value_mlt": [{"resourcetype": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "滋賀県甲西町花園産花こう岩ペグマタイト中のアルカリ長石", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "滋賀県甲西町花園産花こう岩ペグマタイト中のアルカリ長石"}]}, "item_type_id": "2", "owner": "1", "path": ["165"], "permalink_uri": "http://hdl.handle.net/10441/1676", "pubdate": {"attribute_name": "公開日", "attribute_value": "2009-04-13"}, "publish_date": "2009-04-13", "publish_status": "0", "recid": "1707", "relation": {}, "relation_version_is_last": true, "title": ["滋賀県甲西町花園産花こう岩ペグマタイト中のアルカリ長石"], "weko_shared_id": -1}
滋賀県甲西町花園産花こう岩ペグマタイト中のアルカリ長石
http://hdl.handle.net/10441/1676
http://hdl.handle.net/10441/16763e22df29-21b4-4ecd-8375-cb25ffac981d
名前 / ファイル | ライセンス | アクション |
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SJ10_0047_025A.pdf (20.8 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2009-04-13 | |||||
タイトル | ||||||
タイトル | 滋賀県甲西町花園産花こう岩ペグマタイト中のアルカリ長石 | |||||
言語 | ||||||
言語 | jpn | |||||
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 | |||||
著者 |
中野, 聰志
× 中野, 聰志× 江里口, 隆之 |
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著者(ヨミ) | ||||||
姓名 | ナカノ, サトシ | |||||
著者(ヨミ) | ||||||
姓名 | エリグチ, タカユキ | |||||
著者別名 | ||||||
姓名 | Nakano, Satoshi | |||||
著者別名 | ||||||
姓名 | Eriguchi, Takayuki | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Alkali feldspar (Or66Ab33An0.6) in granite pegmatite from Hanazono, Kosei Town, Shiga prefecture, Japan, consists of two parts macroscopically (with the naked eye); one is noncolored and transparent, and another is pinkish and opaque. The latter part ranging from several milimeters to about one centimeter is scattered in the dominant former part. The two parts are microscopically mixed up irregularly in a micron-order, too. The transparent part is clear, and cryptoperthitic of braid-type or lamellar type, or featureless without microtextute, and the pinkish part is turbid and microperthitic of vein-type under an optical microscope. Both the microperthite and braid-cryptoperthite were examined with EPMA , and the size, form and orientation of lamellae or vein, distribution of micropores in both the clear and turbid parts, and compositional variation patterns in microperthitc Ab-rich veins were clrified. The textural features of the alkali feldspar are principally similar to those of the Klokken syenite feldspars. The Klokken model of feldspar cooling, which advocates deuteric coarsening of cryptoperthite to microperthite with micropore formation at the hydrothermal stage in plutonic rocks, may be appllicable to the Hanazono alkali feldspar, in spite of the difference of their bulk compositions. Irregular and complicated Ca distribution patterns in the Hanazono Ab-rich veins, however, throw new insight to the Klokken cooling model. |
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引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 滋賀大学教育学部紀要, 3, 自然科学, 第47号, pp.25-39 | |||||
書誌情報 |
滋賀大学教育学部紀要, 3, 自然科学 号 47, p. 25-39, 発行日 1997 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 1342-9272 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA11123267 | |||||
タイトル(ヨミ) | ||||||
その他のタイトル | シガケン コウセイチョウ ハナゾノサン カコウガン ペグマタイトチュウ ノ アルカリ チョウセキ | |||||
その他の言語のタイトル | ||||||
その他のタイトル | Alkali Feldspar in Granite Pegmatite from Hanazono, Kosei Town, Shiga Prefecture, Japan | |||||
出版者 | ||||||
出版者 | 滋賀大学教育学部 | |||||
資源タイプ | ||||||
内容記述タイプ | Other | |||||
内容記述 | Departmental Bulletin Paper |