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Geothermal conditions in the vilyui basin
Semenov V.P.; Zhelezniak M.N.
发表日期2013
ISSN15607496
卷号17期号:4
英文摘要The characteristics of the geothermal conditions in the Vilyui basin have been adduced. The Vilyui basin is located within the Siberian Platform and contains disequilibrium permafrost. Recently obtained data on permafrost thickness and temperature distribution for geological units of the Vilyui basin have been presented. Estimates of geothermal heat fluxes in and below the permafrost are given. It has been determined that the heat flux in the permafrost is 30-34 mW/m2 lower than in the subpermafrost zone. Four intervals are identified on the temperature curves differing in geothermal gradient and indicating different paleoclimatic conditions in the course of permafrost development. Based on the obtained data, a 2.000 m depth geothermal profile characterizing the geothermal field in the region has been plotted.
英文关键词Geothermal gradient; Geothermal heat flux; Geothermal profile; Ground temperature; Permafrost degradation; Permafrost thickness; Vilyui basin
学科领域geothermal energy; geothermal gradient; heat flux; permafrost; geothermal system; temperature profile; Russian Federation; Siberian Platform; Vilyuy Basin
语种英语
scopus关键词geothermal energy; geothermal gradient; heat flux; permafrost; geothermal system; temperature profile; Russian Federation; Siberian Platform; Vilyuy Basin
来源期刊Earth's Cryosphere
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/120356
作者单位Melnikov Permafrost Institute, SB RAS, Merzlotnaya st., 677010, Yakutsk, Russian Federation
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Semenov V.P.,Zhelezniak M.N.. Geothermal conditions in the vilyui basin[J],2013,17(4).
APA Semenov V.P.,&Zhelezniak M.N..(2013).Geothermal conditions in the vilyui basin.Earth's Cryosphere,17(4).
MLA Semenov V.P.,et al."Geothermal conditions in the vilyui basin".Earth's Cryosphere 17.4(2013).
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