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Volumn 306, Issue 5702, 2004, Pages 1709-1714

In situ evidence for an ancient aqueous environment at Meridiani Planum, Mars

(19)  Squyres, S W a   Grotzinger, J P b   Arvidson, R E c   Bell III, J F a   Calvin, W d   Christensen, P R e   Clark, B C f   Crisp, J A g   Farrand, W H h   Herkenhoff, K E i   Johnson, J R i   Klingelhofer G j   Knoll, A H k   McLennan, S M l   McSween Jr , H Y m   Morris, R V n   Rice Jr , J W e   Rieder, R o   Soderblom, L A i  


Author keywords

[No Author keywords available]

Indexed keywords

EVAPORATION; IRON ORES; MARTIAN SURFACE ANALYSIS; SEDIMENTS; SULFATE MINERALS; WEATHERING;

EID: 10044237708     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.1104559     Document Type: Article
Times cited : (845)

References (39)
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    • (2004) Science , vol.306 , pp. 1698
    • Squyres, S.W.1
  • 2
    • 10044275834 scopus 로고    scopus 로고
    • note
    • Names have been assigned to aerographic features by the Mars Exploration Rover (MER) team for planning and operations purposes. The names are not formally recognized by the International Astronomical Union.
  • 3
    • 10044224479 scopus 로고    scopus 로고
    • J. F. Bell III et al., Science 306, 1703 (2004).
    • (2004) Science , vol.306 , pp. 1703
    • Bell III, J.F.1
  • 4
    • 10044249877 scopus 로고    scopus 로고
    • R. E. Arvidson et al., Science 306, 1730 (2004).
    • (2004) Science , vol.306 , pp. 1730
    • Arvidson, R.E.1
  • 6
    • 10044298294 scopus 로고    scopus 로고
    • R. Rieder et al., Science 306, 1746 (2004).
    • (2004) Science , vol.306 , pp. 1746
    • Rieder, R.1
  • 7
    • 10044233360 scopus 로고    scopus 로고
    • note
    • The term martian soil is used here to denote any loose unconsolidated materials that can be distinguished from rocks, bedrock, or strongly cohesive sediments. No implication of the presence or absence of organic materials or living matter is intended.
  • 13
  • 14
  • 16
    • 0020872458 scopus 로고
    • M. E. Brookfield, T. S. Ahlbrandt, Eds. Elsevier, Amsterdam
    • R. E. Hunter, D. M. Rubin, in Eolian Sediments and Processes, M. E. Brookfield, T. S. Ahlbrandt, Eds. (Elsevier, Amsterdam, 1983), pp. 429-454.
    • (1983) Eolian Sediments and Processes , pp. 429-454
    • Hunter, R.E.1    Rubin, D.M.2
  • 17
    • 0003214620 scopus 로고
    • Society of Economic Paleontologists and Mineralogists, Tulsa, OK
    • J. C. Harms et al., Structures and Sequences in Clastic Rocks (Society of Economic Paleontologists and Mineralogists, Tulsa, OK, 1982).
    • (1982) Structures and Sequences in Clastic Rocks
    • Harms, J.C.1
  • 22
    • 0000280929 scopus 로고
    • Northern Ohio Geological Society, Cleveland
    • L. A. Hardie et al., in Sixth Symposium on Salt (Northern Ohio Geological Society, Cleveland, 1983), pp. 11-39.
    • (1983) Sixth Symposium on Salt , pp. 11-39
    • Hardie, L.A.1
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  • 31
  • 38
    • 10044250535 scopus 로고    scopus 로고
    • note
    • A martian solar day has a mean period of 24 hours 39 min 35244 s and is referred to as a sol to distinguish this from a roughly 3% shorter solar day on Earth.
  • 39
    • 10044284771 scopus 로고    scopus 로고
    • note
    • This research was carried out for the Jet Propulsion Laboratory, California Institute of Technology, under a contract with NASA.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.