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Thermomechanical Waves in the Elastic Lithosphere–Viscous Asthenosphere System
— The problem of the development of thermomechanical waves in the system consisting of two horizontal layers with rheology of a linearly elastic medium for the upper layer (lithosphere) and a viscous fluid for the lower layer (asthenosphere) is considered with regard to phase transition on their com...
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Published in: | Fluid dynamics 2021-11, Vol.56 (6), p.765-779 |
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container_title | Fluid dynamics |
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creator | Lobkovsky, L. I. Ramazanov, M. M. |
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The problem of the development of thermomechanical waves in the system consisting of two horizontal layers with rheology of a linearly elastic medium for the upper layer (lithosphere) and a viscous fluid for the lower layer (asthenosphere) is considered with regard to phase transition on their common boundary. The exact solution to the problem is found and its properties as functions of the parameters are studied. It is shown that for the characteristic physical parameters of the lithosphere and asthenosphere there exist solutions in the form of moderately damped strain tectonic waves and a geophysical interpretation of the results obtained is given. |
doi_str_mv | 10.1134/S0015462821060100 |
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The problem of the development of thermomechanical waves in the system consisting of two horizontal layers with rheology of a linearly elastic medium for the upper layer (lithosphere) and a viscous fluid for the lower layer (asthenosphere) is considered with regard to phase transition on their common boundary. The exact solution to the problem is found and its properties as functions of the parameters are studied. It is shown that for the characteristic physical parameters of the lithosphere and asthenosphere there exist solutions in the form of moderately damped strain tectonic waves and a geophysical interpretation of the results obtained is given.</description><identifier>ISSN: 0015-4628</identifier><identifier>EISSN: 1573-8507</identifier><identifier>DOI: 10.1134/S0015462821060100</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Asthenosphere ; Classical and Continuum Physics ; Classical Mechanics ; Elastic media ; Engineering Fluid Dynamics ; Exact solutions ; Fluid- and Aerodynamics ; Lithosphere ; Parameters ; Phase transitions ; Physical properties ; Physics ; Physics and Astronomy ; Rheological properties ; Rheology ; Tectonics ; Tectonics (Geology) ; Viscous fluids</subject><ispartof>Fluid dynamics, 2021-11, Vol.56 (6), p.765-779</ispartof><rights>Pleiades Publishing, Ltd. 2021. ISSN 0015-4628, Fluid Dynamics, 2021, Vol. 56, No. 6, pp. 765–779. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya RAN. Mekhanika Zhidkosti i Gaza, 2021, Vol. 56, No. 6, pp. 4–18.</rights><rights>COPYRIGHT 2021 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c355t-778d00eae795d34f5706d89e82b52aa328814bceb7f35cf628d3e666ae1a555f3</citedby><cites>FETCH-LOGICAL-c355t-778d00eae795d34f5706d89e82b52aa328814bceb7f35cf628d3e666ae1a555f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27923,27924</link.rule.ids></links><search><creatorcontrib>Lobkovsky, L. I.</creatorcontrib><creatorcontrib>Ramazanov, M. M.</creatorcontrib><title>Thermomechanical Waves in the Elastic Lithosphere–Viscous Asthenosphere System</title><title>Fluid dynamics</title><addtitle>Fluid Dyn</addtitle><description>—
The problem of the development of thermomechanical waves in the system consisting of two horizontal layers with rheology of a linearly elastic medium for the upper layer (lithosphere) and a viscous fluid for the lower layer (asthenosphere) is considered with regard to phase transition on their common boundary. The exact solution to the problem is found and its properties as functions of the parameters are studied. It is shown that for the characteristic physical parameters of the lithosphere and asthenosphere there exist solutions in the form of moderately damped strain tectonic waves and a geophysical interpretation of the results obtained is given.</description><subject>Asthenosphere</subject><subject>Classical and Continuum Physics</subject><subject>Classical Mechanics</subject><subject>Elastic media</subject><subject>Engineering Fluid Dynamics</subject><subject>Exact solutions</subject><subject>Fluid- and Aerodynamics</subject><subject>Lithosphere</subject><subject>Parameters</subject><subject>Phase transitions</subject><subject>Physical properties</subject><subject>Physics</subject><subject>Physics and Astronomy</subject><subject>Rheological properties</subject><subject>Rheology</subject><subject>Tectonics</subject><subject>Tectonics (Geology)</subject><subject>Viscous fluids</subject><issn>0015-4628</issn><issn>1573-8507</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp1kM1KAzEQgIMoWKsP4G3B89Ykm789llJ_oKDQqsclzc52U7qbmmyF3nwH39AnMWULHkTmMDDzfTPDIHRN8IiQjN3OMSacCaoowQITjE_QgHCZpYpjeYoGh3Z66J-jixDWGONcCjpAz4safOMaMLVurdGb5E1_QEhsm3Q1JNONDp01ycx2tQvbyML359erDcbtQjIOkWmP9WS-Dx00l-is0psAV8c8RC9308XkIZ093T9OxrPUZJx3qZSqxBg0yJyXGau4xKJUOSi65FTrjCpF2NLAUlYZN1U8vMxACKGBaM55lQ3RTT936937DkJXrN3Ot3FlQQVmTFGW55Ea9dRKb6CwbeU6r02MEhprXAuVjfWxJIpRklMWBdILxrsQPFTF1ttG-31BcHH4dPHn09GhvRMi267A_57yv_QDHFiAQA</recordid><startdate>20211101</startdate><enddate>20211101</enddate><creator>Lobkovsky, L. I.</creator><creator>Ramazanov, M. M.</creator><general>Pleiades Publishing</general><general>Springer</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20211101</creationdate><title>Thermomechanical Waves in the Elastic Lithosphere–Viscous Asthenosphere System</title><author>Lobkovsky, L. I. ; Ramazanov, M. M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c355t-778d00eae795d34f5706d89e82b52aa328814bceb7f35cf628d3e666ae1a555f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Asthenosphere</topic><topic>Classical and Continuum Physics</topic><topic>Classical Mechanics</topic><topic>Elastic media</topic><topic>Engineering Fluid Dynamics</topic><topic>Exact solutions</topic><topic>Fluid- and Aerodynamics</topic><topic>Lithosphere</topic><topic>Parameters</topic><topic>Phase transitions</topic><topic>Physical properties</topic><topic>Physics</topic><topic>Physics and Astronomy</topic><topic>Rheological properties</topic><topic>Rheology</topic><topic>Tectonics</topic><topic>Tectonics (Geology)</topic><topic>Viscous fluids</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lobkovsky, L. I.</creatorcontrib><creatorcontrib>Ramazanov, M. M.</creatorcontrib><collection>CrossRef</collection><jtitle>Fluid dynamics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lobkovsky, L. I.</au><au>Ramazanov, M. M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Thermomechanical Waves in the Elastic Lithosphere–Viscous Asthenosphere System</atitle><jtitle>Fluid dynamics</jtitle><stitle>Fluid Dyn</stitle><date>2021-11-01</date><risdate>2021</risdate><volume>56</volume><issue>6</issue><spage>765</spage><epage>779</epage><pages>765-779</pages><issn>0015-4628</issn><eissn>1573-8507</eissn><abstract>—
The problem of the development of thermomechanical waves in the system consisting of two horizontal layers with rheology of a linearly elastic medium for the upper layer (lithosphere) and a viscous fluid for the lower layer (asthenosphere) is considered with regard to phase transition on their common boundary. The exact solution to the problem is found and its properties as functions of the parameters are studied. It is shown that for the characteristic physical parameters of the lithosphere and asthenosphere there exist solutions in the form of moderately damped strain tectonic waves and a geophysical interpretation of the results obtained is given.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0015462821060100</doi><tpages>15</tpages></addata></record> |
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subjects | Asthenosphere Classical and Continuum Physics Classical Mechanics Elastic media Engineering Fluid Dynamics Exact solutions Fluid- and Aerodynamics Lithosphere Parameters Phase transitions Physical properties Physics Physics and Astronomy Rheological properties Rheology Tectonics Tectonics (Geology) Viscous fluids |
title | Thermomechanical Waves in the Elastic Lithosphere–Viscous Asthenosphere System |
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