WEKO3
アイテム
{"_buckets": {"deposit": "b7d543a5-197f-4f1a-95eb-e05e3491e673"}, "_deposit": {"created_by": 4, "id": "7772", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "7772"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00007772", "sets": ["957"]}, "author_link": ["428", "12515"], "item_1_alternative_title_5": {"attribute_name": "論文名よみ", "attribute_value_mlt": [{"subitem_alternative_title": "ナンキョク リュツォ・ホルムワン ラングボブデ チイキ ノ チシツ"}]}, "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1974-12", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "17", "bibliographicPageStart": "1", "bibliographicVolumeNumber": "51", "bibliographic_titles": [{"bibliographic_title": "南極資料"}]}]}, "item_1_creator_6": {"attribute_name": "著者名(日)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "石川, 輝海"}, {"creatorName": "イシカワ, テルミ", "creatorNameLang": "ja-Kana"}], "nameIdentifiers": [{"nameIdentifier": "12515", "nameIdentifierScheme": "WEKO"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "ISHIKAWA, Terumi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "428", "nameIdentifierScheme": "WEKO"}]}]}, "item_1_description_1": {"attribute_name": "ページ属性", "attribute_value_mlt": [{"subitem_description": "P(論文)", "subitem_description_type": "Other"}]}, "item_1_description_12": {"attribute_name": "抄録(英)", "attribute_value_mlt": [{"subitem_description": "The rocks exposed in Langhovde, Liitzow-Holm Bay, East Antarctica, are chiefly metamorphic and granitic, with less extensive glacial deposits and beach sediments. Metamorphic rocks consist of metabasite, pyroxene gneiss, hornblende gneiss, garnet-biotite gneiss, porphyroblastic gneiss, garnet gneiss and garnetbearing granitic gneiss. These rocks generally show gentle angle foliation striking northeast and may be Precambrian or possibly Early Paleozoic in age. The metamorphic rocks of Langhovde have a prominent compositional layering or foliation, denned by alternation of quartz-feldspathic, quartzitic, garnetbiotitic or amphibolitic layers of all scales from a fraction of a centimeter to several tens of meters. Foliation is weak in pyroxene gneiss and hornblende gneiss. In the garnet-biotite gneiss and porphyroblastic gneiss, foliation is accentuated by the parallel arrengement of biotite, garnet, feldspars and quartz. The northern part of Langhovde is marked with fold structures, represented by anticlines with an axis of N45°W and synclines with an axis of E-W. In the southern part is found a monoclinal structure striking NE and dipping to the west. Granitic rock is microcline granite, which occurs in the vicinity of Hukuro Cove. The rock is slightly gneissic, pink-colored, and coarse-grained, and it consists mainly of quartz, perthite or perthitic microcline, and biotite, with small amounts of plagioclase and garnet. Glacial deposits are distributed all over the ice-free area, and particularly thick along the boundary between the continental ice and the ice-free area. Immediately overlying the basement is a glacial deposit composed of gneissose rock boulders and cobbles. The boulders are typically rounded and seem to be similar in composition to the underlying basement gneiss. Beach gravel and sand form a terrace along the shore of the inlet and include fossil shells (Adamussium colbecki and Laternula elliptica). ^\u003c14\u003eC age of them shows 3840 ±90 years B.P.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00007772", "subitem_identifier_reg_type": "JaLC"}]}, "item_1_publisher_22": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "国立極地研究所"}]}, "item_1_source_id_13": {"attribute_name": "雑誌書誌ID", "attribute_value_mlt": [{"subitem_source_identifier": "AN00181831", "subitem_source_identifier_type": "NCID"}]}, "item_1_source_id_20": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "00857289", "subitem_source_identifier_type": "ISSN"}]}, "item_1_subject_21": {"attribute_name": "国際十進分類法", "attribute_value_mlt": [{"subitem_subject": "551.1/.4:552", "subitem_subject_scheme": "UDC"}]}, "item_1_text_10": {"attribute_name": "著者所属(英)", "attribute_value_mlt": [{"subitem_text_language": "en", "subitem_text_value": "Department of Earth Sciences, Faculty of Science, Nagoya University"}]}, "item_1_text_2": {"attribute_name": "記事種別(日)", "attribute_value_mlt": [{"subitem_text_value": "研究論文"}]}, "item_1_text_3": {"attribute_name": "記事種別(英)", "attribute_value_mlt": [{"subitem_text_language": "en", "subitem_text_value": "Scientific Paper"}]}, "item_1_text_9": {"attribute_name": "著者所属(日)", "attribute_value_mlt": [{"subitem_text_value": "名古屋大学理学部地球科学教室"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1974-12-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00002476772.pdf", "filesize": [{"value": "9.5 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 9500000.0, "url": {"label": "KJ00002476772", "url": "https://nipr.repo.nii.ac.jp/record/7772/files/KJ00002476772.pdf"}, "version_id": "40bebcf9-1697-4b98-8eda-fe06f4d80cb0"}]}, "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": "南極リュツォ・ホルム湾ラングホブデ地域の地質", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "南極リュツォ・ホルム湾ラングホブデ地域の地質"}, {"subitem_title": "Geology of Langhovde, Lutzow-Holm Bay, East Antarctica", "subitem_title_language": "en"}]}, "item_type_id": "1", "owner": "4", "path": ["957"], "permalink_uri": "https://doi.org/10.15094/00007772", "pubdate": {"attribute_name": "公開日", "attribute_value": "1974-12-01"}, "publish_date": "1974-12-01", "publish_status": "0", "recid": "7772", "relation": {}, "relation_version_is_last": true, "title": ["南極リュツォ・ホルム湾ラングホブデ地域の地質"], "weko_shared_id": 4}
南極リュツォ・ホルム湾ラングホブデ地域の地質
https://doi.org/10.15094/00007772
https://doi.org/10.15094/00007772857ea51b-b7a4-41db-aa89-1d73b35451db
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002476772 (9.5 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1974-12-01 | |||||
タイトル | ||||||
タイトル | 南極リュツォ・ホルム湾ラングホブデ地域の地質 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Geology of Langhovde, Lutzow-Holm Bay, East Antarctica | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00007772 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
記事種別(日) | ||||||
研究論文 | ||||||
記事種別(英) | ||||||
en | ||||||
Scientific Paper | ||||||
論文名よみ | ||||||
その他のタイトル | ナンキョク リュツォ・ホルムワン ラングボブデ チイキ ノ チシツ | |||||
著者名(日) |
石川, 輝海
× 石川, 輝海 |
|||||
著者名(英) |
ISHIKAWA, Terumi
× ISHIKAWA, Terumi |
|||||
著者所属(日) | ||||||
名古屋大学理学部地球科学教室 | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Nagoya University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The rocks exposed in Langhovde, Liitzow-Holm Bay, East Antarctica, are chiefly metamorphic and granitic, with less extensive glacial deposits and beach sediments. Metamorphic rocks consist of metabasite, pyroxene gneiss, hornblende gneiss, garnet-biotite gneiss, porphyroblastic gneiss, garnet gneiss and garnetbearing granitic gneiss. These rocks generally show gentle angle foliation striking northeast and may be Precambrian or possibly Early Paleozoic in age. The metamorphic rocks of Langhovde have a prominent compositional layering or foliation, denned by alternation of quartz-feldspathic, quartzitic, garnetbiotitic or amphibolitic layers of all scales from a fraction of a centimeter to several tens of meters. Foliation is weak in pyroxene gneiss and hornblende gneiss. In the garnet-biotite gneiss and porphyroblastic gneiss, foliation is accentuated by the parallel arrengement of biotite, garnet, feldspars and quartz. The northern part of Langhovde is marked with fold structures, represented by anticlines with an axis of N45°W and synclines with an axis of E-W. In the southern part is found a monoclinal structure striking NE and dipping to the west. Granitic rock is microcline granite, which occurs in the vicinity of Hukuro Cove. The rock is slightly gneissic, pink-colored, and coarse-grained, and it consists mainly of quartz, perthite or perthitic microcline, and biotite, with small amounts of plagioclase and garnet. Glacial deposits are distributed all over the ice-free area, and particularly thick along the boundary between the continental ice and the ice-free area. Immediately overlying the basement is a glacial deposit composed of gneissose rock boulders and cobbles. The boulders are typically rounded and seem to be similar in composition to the underlying basement gneiss. Beach gravel and sand form a terrace along the shore of the inlet and include fossil shells (Adamussium colbecki and Laternula elliptica). ^<14>C age of them shows 3840 ±90 years B.P. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00181831 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00857289 | |||||
書誌情報 |
南極資料 巻 51, p. 1-17, 発行日 1974-12 |
|||||
国際十進分類法 | ||||||
主題Scheme | UDC | |||||
主題 | 551.1/.4:552 | |||||
出版者 | ||||||
出版者 | 国立極地研究所 |