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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">46562</article-id>
   <article-id pub-id-type="doi">10.2205/2020ES000757</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>ORIGINAL ARTICLES</subject>
    </subj-group>
    <subj-group>
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">3D Computer-Assisted Geological Mapping: Testing WinGeol's FaultTrace for semi-automatic structural geological assessment</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>3D Computer-Assisted Geological Mapping: Testing WinGeol's FaultTrace for semi-automatic structural geological assessment</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Faber</surname>
       <given-names>R </given-names>
      </name>
      <name xml:lang="en">
       <surname>Faber</surname>
       <given-names>R </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Domej</surname>
       <given-names>G </given-names>
      </name>
      <name xml:lang="en">
       <surname>Domej</surname>
       <given-names>G </given-names>
      </name>
     </name-alternatives>
     <email>gisela.domej@unimib.it</email>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">TerraMath, Kali Asem</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">TerraMath, Kali Asem</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Universit degli Studi di Milano-Bicocca, Dipartimento di Scienze dell'Ambiente e della Terra</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Universit degli Studi di Milano-Bicocca, Dipartimento di Scienze dell'Ambiente e della Terra</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>21</volume>
   <issue>1</issue>
   <history>
    <date date-type="received" iso-8601-date="2021-10-29T12:48:56+03:00">
     <day>29</day>
     <month>10</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46562/view">https://rjes.ru/en/nauka/article/46562/view</self-uri>
   <abstract xml:lang="ru">
    <p>WinGeol's FaultTrace is a software tool assisting in semi-automatic structural geological mapping of faults and bedding planes. Digital elevation models - such as, for instance, SRTM or ALOS data - are used in combination with satellite imagery for a first structural geological assessment without the requirement of being at the site. Therefore, it is well suited for inaccessible terrain. Borehole data, geological and seismic profiles can be displayed to support the mapping process. Plane elements can be assigned to single as well as to more complex composite geological structures. Moreover, previously mapped data can be densified by interpolation, which is useful to enhance the mapping quality. The tool aims to provide a virtual environment allowing for fast-track and optimized data generation for 3D geological models. The functionality of FaultTrace is demonstrated in two different case studies: The Richãt Structure in Mauritania shows relatively planar fault structures within low-relief topography; the Vineh Structure in Iran shows a complex folding in high mountainous terrain. The studies discuss which structural geological settings let expect a satisfying performance of FaultTrace, and what factors limit the achievement of meaningful results. For the most part, the findings are independent of FaultTrace and, thus, valid for similar software tools.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>WinGeol's FaultTrace is a software tool assisting in semi-automatic structural geological mapping of faults and bedding planes. Digital elevation models - such as, for instance, SRTM or ALOS data - are used in combination with satellite imagery for a first structural geological assessment without the requirement of being at the site. Therefore, it is well suited for inaccessible terrain. Borehole data, geological and seismic profiles can be displayed to support the mapping process. Plane elements can be assigned to single as well as to more complex composite geological structures. Moreover, previously mapped data can be densified by interpolation, which is useful to enhance the mapping quality. The tool aims to provide a virtual environment allowing for fast-track and optimized data generation for 3D geological models. The functionality of FaultTrace is demonstrated in two different case studies: The Richãt Structure in Mauritania shows relatively planar fault structures within low-relief topography; the Vineh Structure in Iran shows a complex folding in high mountainous terrain. The studies discuss which structural geological settings let expect a satisfying performance of FaultTrace, and what factors limit the achievement of meaningful results. For the most part, the findings are independent of FaultTrace and, thus, valid for similar software tools.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>structural geology</kwd>
    <kwd>faults</kwd>
    <kwd>bedding planes</kwd>
    <kwd>3D semi-automatic computer-assisted mapping</kwd>
    <kwd>remote sensing</kwd>
    <kwd>Richãt Structure</kwd>
    <kwd>Karaj Water Conveyance Tunnel</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>structural geology</kwd>
    <kwd>faults</kwd>
    <kwd>bedding planes</kwd>
    <kwd>3D semi-automatic computer-assisted mapping</kwd>
    <kwd>remote sensing</kwd>
    <kwd>Richãt Structure</kwd>
    <kwd>Karaj Water Conveyance Tunnel</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="en">We express our acknowledgments to Dr. S. Sadeghi of the Department of Geology of the Imam Khomeini International University in Tehran, Iran, for having drawn our attention to the interesting geological structures close to Vineh, and for having shared with us digital cartographic work of the area which served as a detailed reference during the software test.</funding-statement>
   </funding-group>
  </article-meta>
 </front>
 <body>
  <p></p>
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