In situ occurrence of Muong Nong-type Australasian tektite fragments from the Quaternary deposits near Huai Om, northeastern Thailand

• 資料種別: 記事
• タイトル: In situ occurrence of Muong Nong-type Australasian tektite fragments from the Quaternary deposits near Huai Om, northeastern Thailand
• 著者・編者: Toshihiro Tada; Ryuji Tada; Praphas Chansom
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2020-11-08
• 出版年（W3CDTF）: 2020-11-08
• タイトル（掲載誌）: Progress in earth and planetary science
• 巻号年月日等（掲載誌）: 7(66)
• 掲載巻: 7(66)
• ISSN（掲載誌）: 2197-4284
• ISSN-L（掲載誌）: 2197-4284
• 本文の言語コード: eng
• DOI: 10.1186/s40645-020-00378-4; https://doi.org/10.1186/s40645-020-00378-4
• 国立国会図書館永続的識別子: info:ndljp/pid/11616308; https://dl.ndl.go.jp/pid/11616308
• コレクション（共通）: 障害者向け資料
• コレクション（障害者向け資料：レベル1）: テキストデータ
• コレクション（個別）: 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他; https://dl.ndl.go.jp/collections/B00035
• 収集根拠: オンライン資料収集制度
• 受理日（W3CDTF）: 2021-01-13T14:13:05+09:00
• 保存日（W3CDTF）: 2021-01-13
• 記録形式（IMT）: application/pdf
• オンライン閲覧公開範囲: 国立国会図書館内限定公開
• デジタル化資料送信: 図書館・個人送信対象外
• 遠隔複写可否（NDL）: 可
• 掲載誌（URI）: https://progearthplanetsci.springeropen.com/articles
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/11467724; https://dl.ndl.go.jp/pid/11467724
• 連携機関・データベース: 国立国会図書館 : 国立国会図書館デジタルコレクション; https://dl.ndl.go.jp

• 要約等: コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
• DOI: 10.1186/s40645-020-00378-4; https://doi.org/10.1186/s40645-020-00378-4
• 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）: http://id.ndl.go.jp/digimeta/11616308; https://dl.ndl.go.jp/pid/11616308; http://link.springer.com/content/pdf/10.1186/s40645-020-00378-4.pdf; http://link.springer.com/article/10.1186/s40645-020-00378-4/fulltext.html
• 参照: Fragment shapes in impact experiments ranging from cratering to catastrophic disruption; https://cir.nii.ac.jp/crid/1050282810831504256; Layered tektites: a multiple impact origin for the Australasian tektites; https://cir.nii.ac.jp/crid/1360011144793359232; Tektites and the Age Paradox in Mid-Pleistocene China; https://cir.nii.ac.jp/crid/1360011145901955712; Mechanism of Muong Nong‐type tektite formation and speculation on the source of Australasian tektites; https://cir.nii.ac.jp/crid/1360292620279483776; Trace element study of high‐ and low‐refractive index Muong Nong‐type tektites from Indochina; https://cir.nii.ac.jp/crid/1360292620507024384; The fractal evolution of particle fragmentation under different fracture energy; https://cir.nii.ac.jp/crid/1360292620949584896; Hydrothermal breccias in vein-type ore deposits: A review of mechanisms, morphology and size distribution; https://cir.nii.ac.jp/crid/1360574096139731328; Coesite in a Muong Nong‐type tektite from Muong Phin, Laos: Description, formation, and survival; https://cir.nii.ac.jp/crid/1360855568648065920; ORIGIN OF INDOCHINITE TEKTITES; https://cir.nii.ac.jp/crid/1360855569187446528; Reaction between water and tektite glass; https://cir.nii.ac.jp/crid/1361137043449601152; Fractals and fragmentation; https://cir.nii.ac.jp/crid/1361137043846332032; Impact fragmentation experiments of basalts and pyrophyllites; https://cir.nii.ac.jp/crid/1361137044318580864; Analysis of Rockfalls by Means of a Fractal Fragmentation Model; https://cir.nii.ac.jp/crid/1361418518499828992; Field recovery of layered tektites in northeast Thailand; https://cir.nii.ac.jp/crid/1361418520714205056; Layered tektites of southeast Asia: Field studies in central Laos and Vietnam; https://cir.nii.ac.jp/crid/1361699995177083776; CONTAMINATION OF SILICIC MAGMAS AND FRACTAL FRAGMENTATION OF XENOLITHS IN PALEOCENE PLUTONS ON KODIAK ISLAND, ALASKA; https://cir.nii.ac.jp/crid/1361981469826231680; Distal Impact Ejecta Layers: Spherules and More; https://cir.nii.ac.jp/crid/1362262944405602176; Quantifying granular material and deformation: Advantages of combining grain size, shape, and mineral phase recognition analysis; https://cir.nii.ac.jp/crid/1362262944889464832; Tektite origin by hypervelocity asteroidal or cometary impact: Target rocks, source craters, and mechanisms; https://cir.nii.ac.jp/crid/1362262945089418240; Geochemistry and origin of Muong Nong-type tektites; https://cir.nii.ac.jp/crid/1362262945490225280; Stretching out the Australasian microtektite strewn field in Victoria Land Transantarctic Mountains; https://cir.nii.ac.jp/crid/1362262946402246272; Do tektites really date the bifaces from the Bose (Baise) Basin, Guangxi, southern China?; https://cir.nii.ac.jp/crid/1362544419685285248; Universality of fragment shapes; https://cir.nii.ac.jp/crid/1362544420667052800; Brazos River bar [Texas]; a study in the significance of grain size parameters; https://cir.nii.ac.jp/crid/1362825894786315520; Source of Australasian tektites: Investigating possible impact sites in Laos; https://cir.nii.ac.jp/crid/1363107368444981120; Fragmentation in the Val Pola rock avalanche, Italian Alps; https://cir.nii.ac.jp/crid/1363107369038263936; In situ fragmentation of lunar blocks and implications for impacts and solar-induced thermal stresses; https://cir.nii.ac.jp/crid/1363107369869769344; Potassium isotope abundances in Australasian tektites and microtektites; https://cir.nii.ac.jp/crid/1363670321070146944; The stratigraphic age of australites revisited; https://cir.nii.ac.jp/crid/1363951794304198400; Excavation and analysis of layered tektites from northeast Thailand: Results of 1994 field expedition; https://cir.nii.ac.jp/crid/1363951794717819136; Sculpturing of moldavites and the problem of micromoldavites; https://cir.nii.ac.jp/crid/1364233268877599488; Fractal analysis and thermal‐elastic modeling of a subvolcanic magmatic breccia: The role of post‐fragmentation partial melting and thermal fracture in clast size distributions; https://cir.nii.ac.jp/crid/1364233268982987904; The oxidation state of iron in tektite glass; https://cir.nii.ac.jp/crid/1364233270530079104
• 参照（URI）: https://cir.nii.ac.jp/crid/1370009142560220553
• 連携機関・データベース: 国立情報学研究所 : CiNii Research; https://cir.nii.ac.jp/
• 提供元機関・データベース: 雑誌記事索引データベース; https://ndlsearch.ndl.go.jp; Crossref; https://www.crossref.org; 科学研究費助成事業データベース; https://kaken.nii.ac.jp/ja
• 書誌ID（NDLBibID）: 11616308; http://id.ndl.go.jp/bib/11616308