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  <front>
    <journal-meta>
      <journal-id journal-id-type="issn">2411-3336</journal-id>
      <journal-id journal-id-type="eissn">2541-9404</journal-id>
      <journal-title-group>
        <journal-title xml:lang="ru">Записки Горного института</journal-title>
        <journal-title xml:lang="en">Journal of Mining Institute</journal-title>
      </journal-title-group>
      <publisher>
        <publisher-name xml:lang="ru">Санкт-Петербургский горный университет императрицы Екатерины ΙΙ</publisher-name>
        <publisher-name xml:lang="en">Empress Catherine II Saint Petersburg Mining University</publisher-name>
      </publisher>
    </journal-meta>
    <article-meta>
      <article-id custom-type="pmi" pub-id-type="custom">pmi-6478</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/6478</article-id>
      <article-categories>
        <subj-group subj-group-type="section-heading" xml:lang="ru">
          <subject>Геология и геофизика</subject>
        </subj-group>
        <subj-group subj-group-type="section-heading" xml:lang="en">
          <subject>Geology and geophsics</subject>
        </subj-group>
      </article-categories>
      <title-group>
        <article-title xml:lang="en">The depth estimation of 2D conductive isometrical bodies by singular points at the tipper frequency characteristic</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>Оценка глубины залегания двумерных электропроводников изометрического сечения по особым точкам частотных характеристик типпера</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="eastern">
            <surname>Ermolin</surname>
            <given-names>E. Yu.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Ермолин</surname>
              <given-names>Е. Ю.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Ermolin</surname>
              <given-names>E. Yu.</given-names>
            </name>
          </name-alternatives>
          <email>ermolin_stud@list.ru</email>
          <xref ref-type="aff" rid="aff1"/>
        </contrib>
        <aff-alternatives id="aff1">
          <aff>
            <institution xml:lang="ru">Санкт-Петербургский государственный горный институт (технический университет) (Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Saint Petersburg State Mining Institute (Technical University) (Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Ingerov</surname>
            <given-names>O. </given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Ингеров</surname>
              <given-names>О. </given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Ingerov</surname>
              <given-names>O. </given-names>
            </name>
          </name-alternatives>
          <email>alingerov@phoenix.com</email>
          <xref ref-type="aff" rid="aff2"/>
        </contrib>
        <aff-alternatives id="aff2">
          <aff>
            <institution xml:lang="ru">Компания «PHOENIX GEOPHYSICS» (Торонто, Канада)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">«PHOENIX GEOPHYSICS» LTD (Toronto, Canada)</institution>
          </aff>
        </aff-alternatives>
      </contrib-group>
      <pub-date pub-type="epub" iso-8601-date="2011-03-21">
        <day>21</day>
        <month>03</month>
        <year>2011</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>2011</year>
      </pub-date>
      <volume>189</volume>
      <fpage>27</fpage>
      <lpage>29</lpage>
      <history>
        <date date-type="received" iso-8601-date="2010-07-29">
          <day>29</day>
          <month>07</month>
          <year>2010</year>
        </date>
        <date date-type="accepted" iso-8601-date="2010-09-02">
          <day>02</day>
          <month>09</month>
          <year>2010</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="2011-03-21">
          <day>21</day>
          <month>03</month>
          <year>2011</year>
        </date>
      </history>
      <permissions>
        <copyright-statement>© E. Yu. Ermolin, O.  Ingerov</copyright-statement>
        <copyright-year>2011</copyright-year>
        <copyright-holder xml:lang="ru">Е. Ю. Ермолин, О.  Ингеров</copyright-holder>
        <copyright-holder xml:lang="en">E. Yu. Ermolin, O.  Ingerov</copyright-holder>
        <license xlink:href="http://creativecommons.org/licenses/by/4.0">
          <license-p>CC BY 4.0</license-p>
        </license>
      </permissions>
      <self-uri xlink:type="simple" xlink:href="https://pmi.spmi.ru/pmi/article/view/6478">https://pmi.spmi.ru/pmi/article/view/6478</self-uri>
      <abstract xml:lang="ru">
        <p>В работе представлен анализ взаимосвязей глубины залегания двумерных проводящих тел с особыми точками частотных характеристик магнитовариационных параметров типпера. Как показали исследования, глубина залегания геометрического центра в рассматриваемом сечении тесно связана с расстоянием между двумя симметричными положительными экстремумами и значениями их амплитуд. Установленные зависимости могут быть использованы как при проектировании поисковых работ, так и при оценке параметров обнаруженных рудных объектов на стадии экспресс-интерпретации полученных данных.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>The relation between parameters of 2D anomaly body and features of vertical sections of tipper amplitude are considered in this paper. According to investigations the depth of center, top and bottom of conductive body is connected with geometrical distance between two symmetrically located positive extremes in tipper pseudo-sections. In addition the tipper amplitude in extremes decreases on account of increasing depth of anomalous body. The described regularities can be used for MT projects planning and quantitative estimation of anomalous body parameters using tipper pseudo-section constructed from field data.</p>
      </abstract>
      <kwd-group xml:lang="ru">
        <title>Ключевые слова</title>
        <kwd>типпрер</kwd>
        <kwd>индукционный вектор</kwd>
        <kwd>двумерные тела</kwd>
      </kwd-group>
      <kwd-group xml:lang="en">
        <title>Keywords</title>
        <kwd>tipper</kwd>
        <kwd>induction arrows</kwd>
        <kwd>two dimensional structures</kwd>
      </kwd-group>
    </article-meta>
  </front>
  <body/>
  <back>
    <ref-list>
      <ref id="ref1">
        <label>1</label>
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  </back>
</article>
