九州南部の大隅花崗閃緑岩体に発達する節理系
デジタルデータあり(科学技術振興機構)
すぐに読む
J-STAGE
全国の図書館の所蔵
国立国会図書館以外の全国の図書館の所蔵状況を表示します。
所蔵のある図書館から取寄せることが可能かなど、資料の利用方法は、ご自身が利用されるお近くの図書館へご相談ください
その他
J-STAGE
デジタルCiNii Research
検索サービスデジタル連携先のサイトで、CiNii Researchが連携している機関・データベースの所蔵状況を確認できます。
書誌情報
この資料の詳細や典拠(同じ主題の資料を指すキーワード、著者名)等を確認できます。
- 資料種別
- 記事
- 著者・編者
- 有留 千博山本 啓司
- 並列タイトル等
- Joint system in the Osumi granodiorite batholith, southern Kyushu, Southwest Japan
- タイトル(掲載誌)
- 地質学雑誌 = The journal of the Geological Society of Japan
- 巻号年月日等(掲載誌)
- 127(8)=1511:2021.8
- 掲載巻
- 127
- 掲載号
- 8
- 掲載通号
- 1511
- 掲載ページ
- 489-495
- 掲載年月日(W3CDTF)
- 2021-08
- ISSN(掲載誌)
- 0016-7630
- ISSN-L(掲載誌)
- 0016-7630
- 出版事項(掲載誌)
- 東京 : 日本地質学会
- 出版地(国名コード)
- JP
- 本文の言語コード
- jpn
- NDLC
- 対象利用者
- 一般
- 所蔵機関
- 国立国会図書館
- 請求記号
- Z15-174
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館雑誌記事索引
- 書誌ID(NDLBibID)
- 031752740
- 整理区分コード
- 632
- 要約等
- <p>This study analyses the joint system of the Middle Miocene Osumi granodiorite batholith in southern Kyushu, Southwest Japan. The analysis included 916 joints at 96 localities covering the northern, middle, and southern domains of the exposed area of the Osumi granodiorite batholith. Two major sets of steep joints striking NNW and ENE and a minor set of gentle joints are recognized in the northern and the middle domains. Two further sets of steep joints striking NS and EW with a minor set of gentle joints are recognized in the southern domain. Previous paleomagnetic studies indicate counterclockwise rotation of microplates in southeast Kyushu after 2 Ma. When the orientations of the joints are restored according to the rotation angles of the microplates (45° for the northern-middle domains and 30° for the southern domain), the strikes of the steep joints are largely oriented NNE and WNW.</p>
- DOI
- 10.5575/geosoc.2021.0018
- オンライン閲覧公開範囲
- インターネット公開
- 連携機関・データベース
- 科学技術振興機構 : J-STAGE
- 要約等
- <p>This study analyses the joint system of the Middle Miocene Osumi granodiorite batholith in southern Kyushu, Southwest Japan. The analysis included 916 joints at 96 localities covering the northern, middle, and southern domains of the exposed area of the Osumi granodiorite batholith. Two major sets of steep joints striking NNW and ENE and a minor set of gentle joints are recognized in the northern and the middle domains. Two further sets of steep joints striking NS and EW with a minor set of gentle joints are recognized in the southern domain. Previous paleomagnetic studies indicate counterclockwise rotation of microplates in southeast Kyushu after 2 Ma. When the orientations of the joints are restored according to the rotation angles of the microplates (45° for the northern-middle domains and 30° for the southern domain), the strikes of the steep joints are largely oriented NNE and WNW.</p>
- DOI
- 10.5575/geosoc.2021.0018
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報(URI)
- 参照
- Strain and stress gradients through the backarc regions of Miocene western Japan: A new type of arc-parallel extensionGeochemical Study of the Osumi Granodiorite, Southwestern Japan
- 参照
- Quantified fracture (joint) clustering in Archean basement, Wyoming: application of the normalized correlation count methodJapan Sea, opening history and mechanism: A synthesisNew insight into a subduction-related orogen: A reappraisal of the geotectonic framework and evolution of the Japanese IslandsStructural Geology AlgorithmsVolcanic history and tectonics of the Southwest Japan ArcPaleogeographic reconstruction and origin of the Philippine SeaIce petrofabric observations from Blue Glacier, Washington, in relation to theory and experimentTranstensional deformation at the junction between the Okinawa trough back-arc basin and the SW Japan island arcPaleomagnetic evidence for post‐Late Miocene intra‐arc rotation of South Kyushu, JapanCircular scanlines and circular windows: new tools for characterizing the geometry of fracture tracesOrigin of the granodiorite in the forearc region of southwest Japan: Melting of the Shimanto accretionary prismCharacterization of natural fracture systems: Analysis of uncertainty effects in linear scanline resultsQuaternary counterclockwise rotation of south Kyushu, southwest JapanTectonics of an arc-arc junction: an example from Kyushu Island at the junction of the Southwest Japan Arc and the Ryukyu ArcU–Pb ages of syenitic and granitic rocks in the Ashizuri igneous complex, southwestern Shikoku: Constraint for the origin of the forarec alkaline magmatism滋賀県"湖南アルプス"における花崗岩中の節理系本邦産火成岩のK-Adating (I)Rb-Srによる地質年令(I)九州南部の中期中新世大隅花崗閃緑岩体における正断層変形とその意義南部九州後期新生代層の花粉層序学的研究Paleomagnetism and Post-Middle Miocene Counter-Clockwise Rotation of Tanegashima Island off Kyushu, Japan.日本の花崗岩:Rb-Sr Whole Rock Ages of the Granites of Minami-osumi and Amami-oshima, Southwest Japan
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- Japan Link Center雑誌記事索引データベースCrossrefCiNii ArticlesCrossrefCrossref
- 書誌ID(NDLBibID)
- 031752740
- NII論文ID
- 130008118753