本文へ移動
九州南部の大隅花崗閃...

九州南部の大隅花崗閃緑岩体に発達する節理系

記事を表すアイコン

九州南部の大隅花崗閃緑岩体に発達する節理系

国立国会図書館請求記号
Z15-174
国立国会図書館書誌ID
031752740
資料種別
記事
著者
有留 千博ほか
出版者
東京 : 日本地質学会
出版年
2021-08
資料形態
掲載誌名
地質学雑誌 = The journal of the Geological Society of Japan 127(8)=1511:2021.8
掲載ページ
p.489-495
詳細を見る

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

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

デジタル

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

デジタル

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>
オンライン閲覧公開範囲
インターネット公開
参照
Strain and stress gradients through the backarc regions of Miocene western Japan: A new type of arc-parallel extension
Geochemical Study of the Osumi Granodiorite, Southwestern Japan
参照
Quantified fracture (joint) clustering in Archean basement, Wyoming: application of the normalized correlation count method
Japan Sea, opening history and mechanism: A synthesis
New insight into a subduction-related orogen: A reappraisal of the geotectonic framework and evolution of the Japanese Islands
Structural Geology Algorithms
Volcanic history and tectonics of the Southwest Japan Arc
Paleogeographic reconstruction and origin of the Philippine Sea
Ice petrofabric observations from Blue Glacier, Washington, in relation to theory and experiment
Transtensional deformation at the junction between the Okinawa trough back-arc basin and the SW Japan island arc
Paleomagnetic evidence for post‐Late Miocene intra‐arc rotation of South Kyushu, Japan
Circular scanlines and circular windows: new tools for characterizing the geometry of fracture traces
Origin of the granodiorite in the forearc region of southwest Japan: Melting of the Shimanto accretionary prism
Characterization of natural fracture systems: Analysis of uncertainty effects in linear scanline results
Quaternary counterclockwise rotation of south Kyushu, southwest Japan
Tectonics of an arc-arc junction: an example from Kyushu Island at the junction of the Southwest Japan Arc and the Ryukyu Arc
U–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
Crossref
CiNii Articles
Crossref
Crossref
書誌ID(NDLBibID)
031752740
NII論文ID
130008118753