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 <front>
  <journal-meta>
   <journal-id journal-id-type="publisher-id">Russian Journal of Earth Sciences</journal-id>
   <journal-title-group>
    <journal-title xml:lang="en">Russian Journal of Earth Sciences</journal-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Russian Journal of Earth Sciences</trans-title>
    </trans-title-group>
   </journal-title-group>
   <issn publication-format="online">1681-1208</issn>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="publisher-id">52759</article-id>
   <article-id pub-id-type="doi">10.2205/2022ES01SI01</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>СПЕЦВЫПУСК: &quot;ФУНДАМЕНТАЛЬНЫЕ И ПРИКЛАДНЫЕ АСПЕКТЫ ГЕОЛОГИИ, ГЕОФИЗИКИ И ГЕОЭКОЛОГИИ&quot;</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>Special Issue: &quot;Fundamental and applied aspects of geology, geophysics and geoecology&quot;</subject>
    </subj-group>
    <subj-group>
     <subject>СПЕЦВЫПУСК: &quot;ФУНДАМЕНТАЛЬНЫЕ И ПРИКЛАДНЫЕ АСПЕКТЫ ГЕОЛОГИИ, ГЕОФИЗИКИ И ГЕОЭКОЛОГИИ&quot;</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">The mathematical model of thermoelastic stresses in the Carpathian region</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>The mathematical model of thermoelastic stresses in the Carpathian region</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Bakhova</surname>
       <given-names>Natalia </given-names>
      </name>
      <name xml:lang="en">
       <surname>Bakhova</surname>
       <given-names>Natalia </given-names>
      </name>
     </name-alternatives>
     <email>bakhova.nataly@gmail.com</email>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">National Academy of Sciences of the Ukraine Institute of geophysics by name S. I. Subbotin</institution>
     <city>Kiev</city>
     <country>Украина</country>
    </aff>
    <aff>
     <institution xml:lang="en">National Academy of Sciences of the Ukraine Institute of geophysics by name S. I. Subbotin</institution>
     <city>Kiev</city>
     <country>Ukraine</country>
    </aff>
   </aff-alternatives>
   <pub-date publication-format="print" date-type="pub" iso-8601-date="2022-12-04T12:06:01+03:00">
    <day>04</day>
    <month>12</month>
    <year>2022</year>
   </pub-date>
   <pub-date publication-format="electronic" date-type="pub" iso-8601-date="2022-12-04T12:06:01+03:00">
    <day>04</day>
    <month>12</month>
    <year>2022</year>
   </pub-date>
   <volume>22</volume>
   <issue>5</issue>
   <fpage>1</fpage>
   <lpage>5</lpage>
   <history>
    <date date-type="received" iso-8601-date="2022-07-01T00:00:00+03:00">
     <day>01</day>
     <month>07</month>
     <year>2022</year>
    </date>
    <date date-type="accepted" iso-8601-date="2022-08-10T00:00:00+03:00">
     <day>10</day>
     <month>08</month>
     <year>2022</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/52759/view">https://rjes.ru/en/nauka/article/52759/view</self-uri>
   <abstract xml:lang="ru">
    <p>The two-dimensional thermoelastic model of the Carpathian region is constructed using the finite element method. The physical-mathematical model is as close as possible to the real environment. A~high-precision detailed distribution of temperatures, heat flow, thermoelastic stresses and displacements is obtained. It is shown that inhomogeneous heating of rocks and structural heterogeneities lead to significant changes in stress and displacement fields in the Carpathian region.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>The two-dimensional thermoelastic model of the Carpathian region is constructed using the finite element method. The physical-mathematical model is as close as possible to the real environment. A~high-precision detailed distribution of temperatures, heat flow, thermoelastic stresses and displacements is obtained. It is shown that inhomogeneous heating of rocks and structural heterogeneities lead to significant changes in stress and displacement fields in the Carpathian region.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>temperature</kwd>
    <kwd>heat flow</kwd>
    <kwd>thermoelastic stresses</kwd>
    <kwd>displacements</kwd>
    <kwd>inhomogeneous medium</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>temperature</kwd>
    <kwd>heat flow</kwd>
    <kwd>thermoelastic stresses</kwd>
    <kwd>displacements</kwd>
    <kwd>inhomogeneous medium</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="ru">temperature, heat flow, thermoelastic stresses, displacements, inhomogeneous medium</funding-statement>
    <funding-statement xml:lang="en">temperature, heat flow, thermoelastic stresses, displacements, inhomogeneous medium</funding-statement>
   </funding-group>
  </article-meta>
 </front>
 <body>
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