Výsledky vyhledávání - "古地磁気学"

Age of Lava Flows in Southwestern Slope of Minamidake, Sakurajima Volcano, Inferred from Paleomagnetic and Chemical Features

Autor: MIKI, Daisuke, UTO, Kozo, HOANG, Nguyen, ISHIHARA, Kazuhiro

Publikováno v: 京都大学防災研究所年報. B. 55:177-181

桜島火山南岳南西斜面の持木川河岸に分布する溶岩流について古地磁気測定および全岩化学組成分析を行った。その結果，9世紀後半から11世紀前半の古地磁気学的推定年代を得た。この�

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=jairo_______::a6924c6b1647ff7bf0b84a44502f2e5d
http://hdl.handle.net/2433/161856

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Equipment for rock magnetic and paleomagnetic study at Aichi University of Education

Publikováno v: 名古屋地学. 72:1-4

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=jairo_______::88da9e8fadbfdcb94238cee38e77380a
http://hdl.handle.net/10424/5195

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Correlation of Lavas on Drilled Cores from the Sakurajima Volcano, Inferred from Paleomagnetic and Chemical Features

Autor: MIKI, Daisuke, UTO, Kozo, SUDO, Masafumi, ISHIHARA, Kazuhiro

Publikováno v: 京都大学防災研究所年報. B. 46:835-840

桜島火山の観測井ボーリングコア中の溶岩や地表に露出する溶岩について蛍光X線法による主要元素組成分析を行った。これらの溶岩の主要元素組成は，コアの全長にわたって一様であっ

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=jairo_______::258a53ab36d0cba2d3a5456fdfe32b19
http://hdl.handle.net/2433/129104

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K-Ar dating and paleomagetic measurements on drilled cores from the Sakurajima volcano - Preliminary attempts to reveal the history of the volcanic activity

Autor: UTO, Kozo, MIKI, Daisuke, UCHIUMI, Shigeru, ISHIHARA, Kazuhiro

Publikováno v: 京都大学防災研究所年報. B. 42(B-1):27-34

桜島火山の黒神, ハルタ山両観測井掘削コアについてK-Ar年代測定と古地磁気測定を行ない, 噴出年代推定を試みた。黒神観測井の3枚の溶岩流は全てAD764年長崎鼻溶岩とほぼ同時期に噴出�

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=jairo_______::1e0c7b1d09ca4ba25a9d40e6e36172b0
http://hdl.handle.net/2433/80399

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Paleomagnetic study for the Oga Peninsula in Northeast Japan

Autor: NISHITANI, Tadashi, TANOUE, Seiji

Publikováno v: 秋田大学鉱山学部資源地学研究施設報告. 53:69-75

Reconstruction of the geological history of the Oga Peninsula in Northeast Japan has been performed. Radiometric dating has been shown that this area had an age of Tertiary and Quaternary.Paleomagnetic analysis revealed that the inclination angle of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=jairo_______::1ab9fba85bd0d84dbaa4066d9dc6360f
http://hdl.handle.net/10295/1118

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