دورية أكاديمية
Climatic and tectonic significance of Taboche Lake, Khumbu Region, Nepal.
العنوان: | Climatic and tectonic significance of Taboche Lake, Khumbu Region, Nepal. |
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المؤلفون: | Gajurel AP; Department of Geology, Tribhuvan University, Kathmandu, Nepal., Hubbard MS; Department of Earth Sciences, Montana State University, Bozeman, MT, USA., Giri B; Department of Earth Sciences, Montana State University, Bozeman, MT, USA., Elmore AC; National Geographic Society, Washington, DC, USA., Maka S; Department of Geology, Tribhuvan University, Kathmandu, Nepal., Rafter PA; University of California, Irvine, CA, USA., Putnam AE; Climate Change Institute, University of Maine, Orono, ME, USA.; School of Earth and Climate Sciences, University of Maine, Orono, ME, USA., Elvin S; National Geographic Society, Washington, DC, USA., Tait A; National Geographic Society, Washington, DC, USA., Mayewski PA; Climate Change Institute, University of Maine, Orono, ME, USA. |
المصدر: | IScience [iScience] 2021 Apr 28; Vol. 24 (5), pp. 102418. Date of Electronic Publication: 2021 Apr 28 (Print Publication: 2021). |
نوع المنشور: | Journal Article |
اللغة: | English |
بيانات الدورية: | Publisher: Cell Press Country of Publication: United States NLM ID: 101724038 Publication Model: eCollection Cited Medium: Internet ISSN: 2589-0042 (Electronic) Linking ISSN: 25890042 NLM ISO Abbreviation: iScience Subsets: PubMed not MEDLINE |
أسماء مطبوعة: | Original Publication: [Cambridge, MA] : Cell Press, [2018]- |
مستخلص: | The Everest region is characterized by its alpine glacial environment. In an effort to understand environmental change and tectonic activity, our team cored Taboche Lake, situated at 4,712 m along the western margin of the Ngozumpa Glacier. This research catalogs past earthquakes using geological records of the lake core that are important for the assessment of future earthquake hazards in the region and provides information for tectonic risk of glacial lake floods. Core grain size characteristics and internal sedimentary structures from computed tomographic scan were coupled with radiocarbon dating of organic matter preserved in the core to reconstruct the environmental history of the area. The 58-cm-long core consists of laminated silty sands and sandy silts with particle diameters <2 mm. The core records a syn-sedimentary deformational structure, folded sediments, rhythmically alternating dark- and light-colored laminations, and turbidites, which indicate coeval climatic and tectonic variations over the past ∼1,600 years. Competing Interests: The authors declare no conflict of interest. (© 2021 The Authors.) |
References: | Science. 2005 Feb 25;307(5713):1302-5. (PMID: 15731452) Science. 1973 Oct 12;182(4108):161-3. (PMID: 17777896) Proc Natl Acad Sci U S A. 2018 Jul 3;115(27):6964-6969. (PMID: 29915076) Nat Commun. 2019 May 21;10(1):2258. (PMID: 31113962) |
فهرسة مساهمة: | Keywords: Glacial Landscapes; Glacial Processes; Sedimentology; Tectonics |
تواريخ الأحداث: | Date Created: 20210611 Latest Revision: 20210612 |
رمز التحديث: | 20221213 |
مُعرف محوري في PubMed: | PMC8169798 |
DOI: | 10.1016/j.isci.2021.102418 |
PMID: | 34113806 |
قاعدة البيانات: | MEDLINE |
تدمد: | 2589-0042 |
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DOI: | 10.1016/j.isci.2021.102418 |