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      <source-app name="Horizon">Horizon</source-app>
      <rec-number>1</rec-number>
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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Lagain, A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Bouley, S.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Baratoux, David</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Costard, F.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Wieczorek, M.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Impact cratering rate consistency test from ages of layered ejecta on Mars</title>
        <secondary-title>Planetary and Space Science</secondary-title>
      </titles>
      <pages>art. 104755 [11 p.]</pages>
      <keywords>
        <keyword>Impact craters</keyword>
        <keyword>Mars</keyword>
        <keyword>Impact rate</keyword>
        <keyword>Layered ejecta craters</keyword>
      </keywords>
      <dates>
        <year>2020</year>
      </dates>
      <call-num>fdi:010077879</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Planetary and Space Science</full-title>
      </periodical>
      <isbn>0032-0633</isbn>
      <accession-num>ISI:000510110900002</accession-num>
      <electronic-resource-num>10.1016/j.pss.2019.104755</electronic-resource-num>
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          <url>https://www.documentation.ird.fr/hor/fdi:010077879</url>
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          <url>https://www.documentation.ird.fr/intranet/publi/2020/02/010077879.pdf</url>
        </pdf-urls>
      </urls>
      <volume>180</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Ages of geological units of planetary bodies are determined from impact crater counts on their surface. These ages are model-dependent, and several models largely used in the community assume a constant production function and a constant cratering rate over the last 3 Ga. We have mapped the population of small impact craters (&gt;200 m in diameter) formed over a population of large impact craters (&gt;5 km in diameter) with layered ejecta on Acidalia Planitia, Mars. We have deduced the age of each large impact crater under the assumption of a constant impact rate and constant production function. The impact rate inferred from this set of ages is, however, not constant and show a significant increasing during the last similar to 1 Ga compared to chronology models commonly used. We interpret this inconsistency as an evidence for temporal variations in the size-frequency distribution (SFD) of impactors in the main belt, consistent with recent studies argued for a late increasing of the large impactor flux on Earth and the Moon.</abstract>
      <custom6>060 ; 020</custom6>
      <custom1>UR234</custom1>
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