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  <controlfield tag="001">4663</controlfield>
  <controlfield tag="005">20200127162937.0</controlfield>
  <datafield tag="037" ind1=" " ind2=" ">
    <subfield code="a">POSTER-2020-0036</subfield>
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  <datafield tag="100" ind1=" " ind2=" ">
    <subfield code="a">Beuthe, Mikael</subfield>
  </datafield>
  <datafield tag="245" ind1=" " ind2=" ">
    <subfield code="a">Titan’s shell thickness</subfield>
  </datafield>
  <datafield tag="260" ind1=" " ind2=" ">
    <subfield code="c">2019</subfield>
  </datafield>
  <datafield tag="269" ind1=" " ind2=" ">
    <subfield code="c">2019-12-10</subfield>
  </datafield>
  <datafield tag="500" ind1=" " ind2=" ">
    <subfield code="a">AGU poster reference: P23D-3523</subfield>
  </datafield>
  <datafield tag="520" ind1=" " ind2=" ">
    <subfield code="a">In a ten year span, the spacecraft Cassini made nine gravity passes among a total of 124 flybys of Titan. The resulting Doppler data have recently been interpreted in terms of a gravity field solution up to harmonic degree and order 5. With its global shape expanded up to degree and order 8, Titan is the icy satellite with the best-known gravity and topography. The simultaneous analysis of these datasets is typically used to constrain the internal structure, in particular the thickness of the icy shell overlying the subsurface ocean. Titan’s gravity anomalies are strongly compensated, which could be explained by a thin shell in isostatic equilibrium, whereas the weak correlation between gravity and topography suggests internal heterogeneities maintained by a sufficiently thick shell. On the basis of these two observations, we shall constrain the thickness of the icy shell.</subfield>
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  <datafield tag="536" ind1=" " ind2=" ">
    <subfield code="a">Belgian PRODEX program managed by ESA in collaboration with the Belgian Federal Science Policy Office/</subfield>
    <subfield code="c">Belgian PRODEX program managed by ESA in collaboration with the Belgian Federal Science Policy Office/</subfield>
    <subfield code="f">Belgian PRODEX program managed by ESA in collaboration with the Belgian Federal Science Policy Office</subfield>
  </datafield>
  <datafield tag="594" ind1=" " ind2=" ">
    <subfield code="a">NO</subfield>
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  <datafield tag="653" ind1="1" ind2=" ">
    <subfield code="a">Titan</subfield>
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  <datafield tag="653" ind1="1" ind2=" ">
    <subfield code="a">gravity</subfield>
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  <datafield tag="653" ind1="1" ind2=" ">
    <subfield code="a">crust</subfield>
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  <datafield tag="653" ind1="1" ind2=" ">
    <subfield code="a">moment of inertia</subfield>
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  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Rivoldini, Attilio</subfield>
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  <datafield tag="773" ind1=" " ind2=" ">
    <subfield code="t">American Geophysical Union Fall Meeting 2019, San Francisco</subfield>
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  <datafield tag="856" ind1="0" ind2=" ">
    <subfield code="f">mikael.beuthe@observatoire.be</subfield>
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  <datafield tag="856" ind1="4" ind2="2">
    <subfield code="a">https://agu.confex.com/agu/fm19/meetingapp.cgi/Paper/493030</subfield>
  </datafield>
  <datafield tag="980" ind1=" " ind2=" ">
    <subfield code="a">CPOSTER</subfield>
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