Two times lowering of lake water at around 48 and 38 ka, caused by possible earthquakes, recorded in the Paleo-Kathmandu lake, central Nepal Himalaya

• Material Type: 記事
• Title: Two times lowering of lake water at around 48 and 38 ka, caused by possible earthquakes, recorded in the Paleo-Kathmandu lake, central Nepal Himalaya
• Author/Editor: Harutaka Sakai; Rie Fujii; Misa Sugimoto
• Publication, Distribution, etc.: 日本 : Springer science+business media
• Publication Date: 2016-02-27
• Publication Date (W3CDTF): 2016-02-27
• Periodical title: EPS : Earth, Planets and Space
• No. or year of volume/issue: 68(31)
• Volume: 68(31)
• ISSN (Periodical Title): 1880-5981
• ISSN-L (Periodical Title): 1343-8832
• Text Language Code: eng
• DOI: 10.1186/s40623-016-0413-5; https://doi.org/10.1186/s40623-016-0413-5
• Persistent ID (NDL): info:ndljp/pid/9976773; https://dl.ndl.go.jp/pid/9976773
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• Date Accepted (W3CDTF): 2016-05-17T18:44:59+09:00
• Date Captured (W3CDTF): 2016-05-17
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• Periodical Title (URI): http://earth-planets-space.springeropen.com/articles?searchType=journalSearch&sort=PubDate&page=2
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• Bibliographic ID (NDL): 9976773; http://id.ndl.go.jp/bib/9976773
• Bibliographic Record Category (NDL): 632

• Summary, etc.: Sedimentary facies and micro-fossil analyses, and AMS[14]C dating were performed in order to reveal the water-level fall events and draining process of the lake (Paleo-Kathmandu Lake) that existed in the past in the Central Nepal Himalaya. The sedimentary facies change from the lacustrine Kalimati Formation to the deltaic Sunakothi Formation in the southern and central Kathmandu basin, and the abrupt and prominent increase of phytoliths Bambusoideae and Pediastrum, and contemporaneous decrease of sponge spicule and charcoal grains around 48 and 38 ka support the lowering of water level at these times. According to the pollen analysis, both events occurred under rather warm and wet climate, thus supporting that they were triggered by tectonic cause and not by climate change. The first event might be linked to a possible occurrence of a large earthquake with an epicenter in the vicinity of the Paleo-Kathmandu Lake. The occurrence of a mega landslide in Langtang area close to the north of the Kathmandu Valley producing pseudotachylite dated at 51 ± 13 ka could be linked to this earthquake. Finally, the water was completely drained out from the remnant lake at the central part of the Kathmandu basin by ca.12 ka.
• DOI: 10.1186/s40623-016-0413-5; https://doi.org/10.1186/s40623-016-0413-5
• Access Restrictions: インターネット公開
• Rights (production): © 2016 Sakai et al. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
• Related Material (URI): http://hdl.handle.net/2433/212439; http://id.ndl.go.jp/digimeta/9976773; https://dl.ndl.go.jp/pid/9976773; http://link.springer.com/content/pdf/10.1186/s40623-016-0413-5.pdf; http://link.springer.com/article/10.1186/s40623-016-0413-5/fulltext.html; http://link.springer.com/content/pdf/10.1186/s40623-016-0413-5
• Is Referenced By: Examination of shallow and deep S-wave velocity structures from microtremor array measurements and receiver function analysis at strong-motion stations in Kathmandu basin, Nepal; https://cir.nii.ac.jp/crid/1050306506449935744; Three-dimensional velocity structure models in and around the Kathmandu Valley, Central Nepal; https://cir.nii.ac.jp/crid/1360021390583827072; 2015年ネパール・ゴルカ地震による高速道路盛土部とその周辺部の亀裂及び段差の発生原因に関する考察; https://cir.nii.ac.jp/crid/1390845713015328128; Special issue "the 2015 Gorkha, Nepal, earthquake and Himalayan studies : First results"; https://cir.nii.ac.jp/crid/2050588891960741120
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• Bibliographic ID (NDL): 9976773; http://id.ndl.go.jp/bib/9976773
• NAID: 120005758191