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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">67008</article-id>
   <article-id pub-id-type="doi">10.2205/2023ES000874</article-id>
   <article-id pub-id-type="edn">htcabo</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">Subsidence and sedimentation dynamics of the lakeside part of the Rita River delta in the rupture zone, the northwestern coast of Lake Baikal</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Динамика оседания и осадконакопления приозерной части дельты р. Риты в зоне разрывов на северо-западном побережье оз. Байкал</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-7743-8877</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Лунина</surname>
       <given-names>Оксана Викторовна</given-names>
      </name>
      <name xml:lang="en">
       <surname>Lunina</surname>
       <given-names>Oksana Viktorovna</given-names>
      </name>
     </name-alternatives>
     <email>lounina@inbox.ru</email>
     <bio xml:lang="ru">
      <p>доктор геолого-минералогических наук;</p>
     </bio>
     <bio xml:lang="en">
      <p>doctor of geological and mineralogical sciences;</p>
     </bio>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-4235-6745</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Гладков</surname>
       <given-names>Антон Андреевич</given-names>
      </name>
      <name xml:lang="en">
       <surname>Gladkov</surname>
       <given-names>Anton Andreevich</given-names>
      </name>
     </name-alternatives>
     <email>anton90ne@rambler.ru</email>
     <bio xml:lang="ru">
      <p>кандидат геолого-минералогических наук;</p>
     </bio>
     <bio xml:lang="en">
      <p>candidate of geological and mineralogical sciences;</p>
     </bio>
     <xref ref-type="aff" rid="aff-2"/>
     <xref ref-type="aff" rid="aff-3"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Институт земной коры СО РАН</institution>
     <city>Иркутск</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Institute of the Earth’s Crust, Siberian Branch of Russian Academy of Sciences</institution>
     <city>Irkutsk</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Институт земной коры СО РАН</institution>
     <city>Иркутск</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Institute of the Earth’s Crust, Siberian Branch of Russian Academy of Sciences</institution>
     <city>Иркутск</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-3">
    <aff>
     <institution xml:lang="ru">ГАУ ДО ИО &quot;Центр развития дополнительного образования детей&quot;</institution>
     <city>Иркутск</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Center for the Development of Continuing Education of Children, Ministry of Education of Irkutsk Region</institution>
     <city>Иркутск</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <pub-date publication-format="print" date-type="pub" iso-8601-date="2023-12-30T00:00:00+03:00">
    <day>30</day>
    <month>12</month>
    <year>2023</year>
   </pub-date>
   <pub-date publication-format="electronic" date-type="pub" iso-8601-date="2023-12-30T00:00:00+03:00">
    <day>30</day>
    <month>12</month>
    <year>2023</year>
   </pub-date>
   <volume>23</volume>
   <issue>6</issue>
   <fpage>1</fpage>
   <lpage>18</lpage>
   <history>
    <date date-type="received" iso-8601-date="2023-06-30T00:00:00+03:00">
     <day>30</day>
     <month>06</month>
     <year>2023</year>
    </date>
    <date date-type="accepted" iso-8601-date="2023-09-22T00:00:00+03:00">
     <day>22</day>
     <month>09</month>
     <year>2023</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/67008/view">https://rjes.ru/en/nauka/article/67008/view</self-uri>
   <abstract xml:lang="ru">
    <p>В связи с активным освоением речных дельт их оседание является одной из ключевых проблем жизнедеятельности человека. Процесс закономерный и зависит от многих факторов, влияние которых еще недостаточно изучено. Нами проведено исследование, цель которого заключалась в выявлении изменений земной поверхности приозерной части дельты р. Риты в зоне ранее выявленных разрывов на северо-западном побережье оз. Байкал. Оценка топографических изменений выполнялась путем расчета разницы между разновременными цифровыми моделями местности (ЦММ), полученными на двух локальных участках по данным беспилотной аэрофотосъемки сверхвысокого разрешения в 2020 и 2021 гг. В результате установлено, что оседание приозерной части дельты за 11 месяцев и 19 дней произошло в среднем на 5–10 см. Эти значения ассоциируются с естественным уплотнением осадков. В местах их накопления агградация происходит на аналогичные величины, уравновешивая баланс отложений. В выходах сейсмогравитационных нарушений в отсутствии наносов просадки достигли 33–37 см, что указывает на активные эндогенные и экзогенные процессы в зоне Кочериковского разлома. Наибольшие отрицательные и положительные вертикальные изменения рельефа до 40 см произошли в пределах пляжа и связаны с волноприбойной деятельностью. Самая крайняя заболоченная часть мыса Рытого испытала максимальное опускание за год. Наибольшее накопление аллювия произошло на южном участке дельты р. Риты в понижении, выраженном в рельефе местности и совпадающим с зоной современных разрывов, а также в аккумулятивном потоке, перекрывающем зону поверхностных нарушений. За исключением этой части, несмотря на интенсивные наносы, разрывы хорошо проявлены на ЦММ, а значит, продолжают развиваться. Сравнение разновременных ЦММ путем вычитания высотных отметок для каждого узла (пикселя) модели является перспективным и недорогим методом для целей мониторинга деформаций земной поверхности.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>Delta subsidence is one of the key problems of human life as these areas are developed quite fast. The process is natural and depends on many factors, the influence of which has not yet been sufficiently studied. This study is aimed to identify changes in the earth’s surface of the lakeside part of the Rita River delta on the northwestern coast of Lake Baikal, where a zone of seismically induced gravitational ruptures were recently mapped. To assess topographic changes, we used the calculation of the difference in multi-temporal digital surface models (DSM) obtained in two local areas from ultra-high resolution unmanned aerial photography in 2020 and 2021. We established that the subsidence of the lakeside part of the delta occurred on average by 5–10 cm over 11 months and 19 days. These values are associated with natural sediment compaction. In places of their accumulation, aggradation occurs by similar values, compensating the balance of deposits. In the seismically induced gravitational failures in the absence of alluvium, subsidence reached 33–37 cm, which indicates active endogenous and exogenous processes in the Kocherikovsky fault zone. The largest negative and positive vertical topographic changes up to 40 cm occurred within the beach and were associated with wave-cutting activity. The most extreme swampy part of Cape Rytyi experienced the maximum subsidence per a year. The greatest accumulation of alluvium occurred in the southern section of the Rita River delta in a settling expressed in the surface and coinciding with the zone of recent ruptures, as well as in an accumulative flow that overlaps the zone of surface deformations. With the exception of this part, discontinuities are well exhibited on DSM that means they continue to develop despite intensive sedimentation. Comparison of multi-temporal DSM and DTM by calculating the difference in elevation for each node (pixel) of the model is a promising and inexpensive method for monitoring surface deformations.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>зона разрывов</kwd>
    <kwd>дельта</kwd>
    <kwd>оседание</kwd>
    <kwd>беспилотная аэрофотосъемка</kwd>
    <kwd>цифровая модель местности</kwd>
    <kwd>Байкал</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>rupture zone</kwd>
    <kwd>delta</kwd>
    <kwd>subsidence</kwd>
    <kwd>unmanned aerial system</kwd>
    <kwd>digital surface model</kwd>
    <kwd>Baikal</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="ru">Авторы благодарны Е. Б. Игнатенко за помощь при подготовке рисунков. Работы выполнены в рамках государственного задания Института земной коры Сибирского отделения Российской академии наук на 2021–2025 гг. «Современная геодинамика, механизмы деструкции литосферы и опасные геологические процессы в Центральной Азии» (проект № FWEF-2021-0009), с использованием оборудования и инфраструктуры уникальной научной установки «Южно-Байкальский инструментальный комплекс для мониторинга опасных геодинамических процессов» Центра коллективного пользования «Геодинамика и геохронология» ИЗК СО РАН по гранту № 075-15-2021-682. Работы проведены при сотрудничестве с ФГБУ «Заповедное Прибайкалье», предоставившего возможность выполнения научно-исследовательских работ на территории Байкало-Ленского заповедника в рамках договора № 43 от 30.05.2019 г.</funding-statement>
    <funding-statement xml:lang="en">The authors are grateful to E. B. Ignatenko for help in preparing the drawings. The work was carried out within the framework of the state assignment of the Institute of the Earth's Crust of the Siberian Branch of the Russian Academy of Sciences for 2021–2025. “Modern geodynamics, mechanisms of destruction of the lithosphere and hazardous geological processes in Central Asia” (project No. FWEF-2021-0009), using the equipment and infrastructure of the unique scientific installation “South Baikal instrumental complex for monitoring hazardous geodynamic processes” of the Center for Collective Use “Geodynamics” and geochronology&quot; from the Institute of Culture SB RAS under grant No. 075-15-2021-682. The work was carried out in collaboration with the Federal State Budgetary Institution “Reserve Pribaikalye”, which provided the opportunity to carry out research work on the territory of the Baikal-Lena Nature Reserve under agreement No. 43 of May 30, 2019.</funding-statement>
   </funding-group>
  </article-meta>
 </front>
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