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Volumn 50, Issue 9, 2002, Pages 903-913

Development and testing of subsurface sampling devices for the Beagle 2 lander

Author keywords

Beagle 2; Lander; Mars; Rock; Sampling device; Soil

Indexed keywords

MARTIAN SURFACE ANALYSIS; METEORITES; SOILS; ULTRAVIOLET RADIATION;

EID: 0036701534     PISSN: 00320633     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0032-0633(02)00066-1     Document Type: Article
Times cited : (85)

References (13)
  • 1
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    • Nature and origin of Martian surface materials
    • Abstract, 6017
    • Bell, J.F. III, 1999. Nature and origin of Martian surface materials. Fifth International Mars Conference, Abstract, 6017.
    • (1999) Fifth International Mars Conference
    • Bell J.F. III1
  • 4
    • 0012492003 scopus 로고    scopus 로고
    • Craters as an indicator of Martian regolith thickness
    • Abstract, 6228
    • Gilmore, M.S., 1999. Craters as an indicator of Martian regolith thickness. Fifth International Mars Conference, Abstract, 6228.
    • (1999) Fifth International Mars Conference
    • Gilmore, M.S.1
  • 6
    • 0001076252 scopus 로고
    • The Viking biological experiments on Mars
    • Klein H.P. The Viking biological experiments on Mars. Icarus. 34:1978;666-674.
    • (1978) Icarus , vol.34 , pp. 666-674
    • Klein, H.P.1
  • 8
    • 0034623764 scopus 로고    scopus 로고
    • Sedimentary rocks of early Mars
    • Malin M.C., Edgett K.S. Sedimentary rocks of early Mars. Science. 290(5498):2000;1927-1937.
    • (2000) Science , vol.290 , Issue.5498 , pp. 1927-1937
    • Malin, M.C.1    Edgett, K.S.2
  • 9
    • 0003217956 scopus 로고
    • Physical properties of surface materials
    • D. Kaplan (comp.). NASA TM 100470
    • Moore, H., 1988. Physical properties of surface materials. In: D. Kaplan (comp.), Environment of Mars. NASA TM 100470.
    • (1988) Environment of Mars
    • Moore, H.1
  • 13
    • 0034665930 scopus 로고    scopus 로고
    • Evidence that the reactivity of the Martian soil is due to superoxide ions
    • Yen A.S., Kim S.S., Hecht M.H., Frant M.S., Murray B. Evidence that the reactivity of the Martian soil is due to superoxide ions. Science. 289:2000;1909-1912.
    • (2000) Science , vol.289 , pp. 1909-1912
    • Yen, A.S.1    Kim, S.S.2    Hecht, M.H.3    Frant, M.S.4    Murray, B.5


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.