HUSCAP logo Hokkaido Univ. logo

Hokkaido University Collection of Scholarly and Academic Papers >
共同研究拠点  >
21世紀COEプログラム「新・自然史科学創成」  >
Origin and Evolution of Natural Diversity >
Proceedings >

Rockmagnetic Characterization of the Setana and Chiraigawa Formations in SW Hokkaido (Soebetsu River, Kuromatsunai)

フルテキスト
p101-107-origin08.pdf1.09 MBPDF見る/開く
この文献へのリンクには次のURLを使用してください:http://hdl.handle.net/2115/38445

タイトル: Rockmagnetic Characterization of the Setana and Chiraigawa Formations in SW Hokkaido (Soebetsu River, Kuromatsunai)
著者: Gautam, Pitambar 著作を一覧する
Takashima, Reishi 著作を一覧する
Dick, Matthew H. 著作を一覧する
Kanamatsu, Toshiya 著作を一覧する
Rijal, Moti L. 著作を一覧する
Nishi, Hiroshi 著作を一覧する
Mawatari, Shunsuke F. 著作を一覧する
キーワード: Magnetic susceptibility
Rock magnetism
Curie temperature
Setana Formation
Hokkaido
発行日: 2008年
出版者: 21st Century COE for Neo-Science of Natural History, Hokkaido University
引用: Edited by Hisatake Okada, Shunsuke F. Mawatari, Noriyuki Suzuki, Pitambar Gautam. ISBN: 978-4-9903990-0-9
誌名: Origin and Evolution of Natural Diversity : Proceedings of the International Symposium, The Origin and Evolution of Natural Diversity, held from 1-5 October 2007 in Sapporo, Japan
開始ページ: 101
終了ページ: 107
抄録: Rockmagnetic investigations were conducted on sediments constituting the upper part of the Setana Formation and the Chiraigawa Formation, of Plio-Pleistocene age, exposed along the Soebetsu River in the vicinity of Kuromatsunai town, Hokkaido. Average mass-specific low-field magnetic susceptibility (χ) had the lowest value (15.2 x 10^[-8] m^3kg^[-1]) at one site in the Kuromatsunai Formation, but higher values represented by wide ranges of (26.1-132.2) x 10^[-8] m^3kg^[-1] and (135.6-870.1) x 10^[-8] m^3kg^[-1] characterized the Chiraigawa and Setana Formations, respectively. Magnetomineralogical analyses by isothermal remanence (IRM) acquisition, Curie temperature determinations, and electron microscopy aided with energy dispersive X-ray analysis suggest the presence of several types of magnetic minerals: (i) one of a soft coercivity phase, probably a Ti-poor magnetite, with a Curie temperature of ca. 535-555℃, occurring throughout the section; (ii) one of intermediate coercivity, relatively rich in Ti (ca. 10% by weight), with a Curie temperature of ca. 460-475℃, restricted to two relatively thin layers of the Chiraigawa Formation, each several tens of cm thick; and (iii) a hard-coercivity hematite-like and/or a very-hard-coercivity goethite-like phase contributing up to 0.5-5% of the saturation IRM acquired at 2.5 T. Combined use of susceptibility and several ratios or differences derived from IRM acquisition data, bi-plots of IRM vs. χ, and magnetomineralogical inferences were used to discriminate rockmagnetic zones within the Soebetsu River Section. Similar rockmagnetic analyses have proven to be effecive for mapping as well as for lithostratigraphical correlations of geological sections. Combined use of these rockmagnetic zones with other environment/climate proxy data may prove effective in paleoenvironmental reconstruction.
記述: International Symposium, "The Origin and Evolution of Natural Diversity". 1–5 October 2007. Sapporo, Japan.
資料タイプ: proceedings
URI: http://hdl.handle.net/2115/38445
出現コレクション:Proceedings

提供者: Gautam Pitambar

 

本サイトに関するご意見・お問い合わせは repo at lib.hokudai.ac.jp へお願いします。 - 北海道大学