Permittivity estimation of layers beneath the northern polar layered deposits, Mars (Articolo in rivista)

Type
Label
  • Permittivity estimation of layers beneath the northern polar layered deposits, Mars (Articolo in rivista) (literal)
Anno
  • 2010-01-01T00:00:00+01:00 (literal)
Alternative label
  • Lauro SE, Mattei E, Pettinelli E, Soldovieri F, Orosei R, Cartacci M, Cicchetti A, Noschese R, Giuppi S (2010)
    Permittivity estimation of layers beneath the northern polar layered deposits, Mars
    in Geophysical research letters
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Lauro SE, Mattei E, Pettinelli E, Soldovieri F, Orosei R, Cartacci M, Cicchetti A, Noschese R, Giuppi S (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 37 (literal)
Rivista
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Univ Roma Tre, Dept Phys E Amaldi, I-00146 Rome, Italy CNR, Inst Electromagnet Sensing Environm, I-80124 Naples, Italy Ist Nazl Astrofis, Ist Fis Spazio Interplanetario, I-00133 Rome, Italy (literal)
Titolo
  • Permittivity estimation of layers beneath the northern polar layered deposits, Mars (literal)
Abstract
  • Martian Polar Layered Deposits, most likely dusty ice are transparent to radar waves. In the North Pole bedrock has been detected by MARSIS up to a depth about 2 Km, whereas in the South Pole such interface has been located at about 3.7 Km. The reflected signal is generally above the noise and can be used to estimate the dielectric properties of the bedrock. Assuming the permittivity of the first layer is known, we use a simplified inversion method to extract the bedrock relative dielectric permittivity as 4-9 below the North PLD's. These values are coherent with the basalt nature and so the approach could be used to identify the lithology beneath the Martian Poles. (literal)
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