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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">46899</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">A new technique for recognizing fractured zones in P-P reflection fields, applied to the study of a North Sea oil reservoir</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>A new technique for recognizing fractured zones in P-P reflection fields, applied to the study of a North Sea oil reservoir</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Semerikova</surname>
       <given-names>Irina I </given-names>
      </name>
      <name xml:lang="en">
       <surname>Semerikova</surname>
       <given-names>Irina I </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Evans</surname>
       <given-names>J Russ</given-names>
      </name>
      <name xml:lang="en">
       <surname>Evans</surname>
       <given-names>J Russ</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Booth</surname>
       <given-names>David C </given-names>
      </name>
      <name xml:lang="en">
       <surname>Booth</surname>
       <given-names>David C </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-3"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Dai</surname>
       <given-names>Hengchang </given-names>
      </name>
      <name xml:lang="en">
       <surname>Dai</surname>
       <given-names>Hengchang </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-4"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Blinova</surname>
       <given-names>Tatiana S </given-names>
      </name>
      <name xml:lang="en">
       <surname>Blinova</surname>
       <given-names>Tatiana S </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-5"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Organization of the Russian Academy of Sciences Mining Institute of the Ural Branch of the RAS, Perm, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Organization of the Russian Academy of Sciences Mining Institute of the Ural Branch of the RAS, Perm, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">British Geological Survey, Edinburgh, UK</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">British Geological Survey, Edinburgh, UK</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-3">
    <aff>
     <institution xml:lang="ru">British Geological Survey, Edinburgh, UK</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">British Geological Survey, Edinburgh, UK</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-4">
    <aff>
     <institution xml:lang="ru">British Geological Survey, Edinburgh, UK</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">British Geological Survey, Edinburgh, UK</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-5">
    <aff>
     <institution xml:lang="ru">Organization of the Russian Academy of Sciences Mining Institute of the Ural Branch of the RAS, Perm, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Organization of the Russian Academy of Sciences Mining Institute of the Ural Branch of the RAS, Perm, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>12</volume>
   <issue>5</issue>
   <fpage>1</fpage>
   <lpage>10</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-11-10T01:06:02+03:00">
     <day>10</day>
     <month>11</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46899/view">https://rjes.ru/en/nauka/article/46899/view</self-uri>
   <abstract xml:lang="ru">
    <p>A technique is presented for recognizing different types of fractured zones within the internal subsurface structure, including zones of extended fractures with dimensions larger than the signal wavelength, and zones of small differently oriented fractures with dimensions smaller than the signal wavelength. The technique is based on dynamic analysis, using prospecting indicators for fractures and faults of different classes, determined from the dynamic parameters of P-P reflections. These prospecting indicators are determined from the results of seismic modeling, as well as physical modeling with samples of natural rock and field seismic surveys on known fractured objects with fracture parameters in different lithologic rock types. We have studied the quality, stability and statistical significance of the indicators, and on the basis of the dynamic analysis we determine the probability of the presence of fractured objects of a particular type. The resulting technique has been applied to a fractured hydrocarbon reservoir under the North Sea, where it has been possible to better determine the particular features of its geologic structure. Fractured zones in a gas-saturated unstratified subsurface have been mapped; possible large tectonic faults and block structure have been revealed; results show the likely presence of diffracting objects within the rock matrix, determine their type, and improve the imaging of reflecting horizons with weak intensity and fragmented correlation.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>A technique is presented for recognizing different types of fractured zones within the internal subsurface structure, including zones of extended fractures with dimensions larger than the signal wavelength, and zones of small differently oriented fractures with dimensions smaller than the signal wavelength. The technique is based on dynamic analysis, using prospecting indicators for fractures and faults of different classes, determined from the dynamic parameters of P-P reflections. These prospecting indicators are determined from the results of seismic modeling, as well as physical modeling with samples of natural rock and field seismic surveys on known fractured objects with fracture parameters in different lithologic rock types. We have studied the quality, stability and statistical significance of the indicators, and on the basis of the dynamic analysis we determine the probability of the presence of fractured objects of a particular type. The resulting technique has been applied to a fractured hydrocarbon reservoir under the North Sea, where it has been possible to better determine the particular features of its geologic structure. Fractured zones in a gas-saturated unstratified subsurface have been mapped; possible large tectonic faults and block structure have been revealed; results show the likely presence of diffracting objects within the rock matrix, determine their type, and improve the imaging of reflecting horizons with weak intensity and fragmented correlation.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Reservoir geophysics</kwd>
    <kwd>parameter estimation</kwd>
    <kwd>modelling</kwd>
    <kwd>wave interpretation</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Reservoir geophysics</kwd>
    <kwd>parameter estimation</kwd>
    <kwd>modelling</kwd>
    <kwd>wave interpretation</kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <p></p>
 </body>
 <back>
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</article>
