The scientific rationale for the C1XS X-ray spectrometer on India's Chandrayaan-1 mission to the moon

被引:28
作者
Crawford, I. A. [1 ]
Joy, K. H. [1 ,2 ,3 ]
Kellett, B. J. [2 ]
Grande, M. [4 ]
Anand, M. [3 ,5 ]
Bhandari, N. [6 ]
Cook, A. C. [4 ]
d'Uston, L. [7 ]
Fernandes, V. A. [8 ]
Gasnault, O. [7 ]
Goswami, J. [6 ]
Howe, C. J. [2 ]
Huovelin, J. [9 ]
Koschny, D.
Lawrence, D. J. [10 ]
Maddison, B. J. [2 ]
Maurice, S. [7 ]
Narendranath, S. [11 ]
Pieters, C. [12 ]
Okada, T. [13 ]
Rothery, D. A. [5 ]
Russell, S. S. [3 ]
Sreekumar, P. [11 ]
Swinyard, B. [2 ]
Wieczorek, M. [14 ]
Wilding, M. [4 ]
机构
[1] Birkbeck UCL Res Sch Earth Sci, Ctr Planetary Sci, London WC1E 6BT, England
[2] Rutherford Appleton Lab, Space Sci & Technol Dept, Didcot OX11 0QX, Oxon, England
[3] Nat Hist Museum, Dept Mineral, London SW7 5BD, England
[4] Univ Wales, Inst Math & Phys Sci, Aberystwyth SY23 3BZ, Dyfed, Wales
[5] Open Univ, Dept Earth & Environm Sci, Milton Keynes MK7 6AA, Bucks, England
[6] Phys Res Lab, Ahmadabad 380009, Gujarat, India
[7] CNRS UPS, Ctr Etud Spatiale Rayonnements, Toulouse, France
[8] Berkeley Geochronol Ctr, Berkeley, CA USA
[9] Univ Helsinki, FI-00014 Helsinki, Finland
[10] Johns Hopkins Univ, Appl Phys Lab, Baltimore, MD 21218 USA
[11] Indian Space Res Org, Bangalore 562140, Karnataka, India
[12] Brown Univ, Providence, RI 02912 USA
[13] Japan Aerosp Explorat Agcy, Inst Space & Astronaut Sci, Kanagawa 2298510, Japan
[14] Inst Phys Globe Paris, Paris, France
关键词
Moon; Lunar science; X-ray spectroscopy; LUNAR METEORITE; SMART-1; MISSION; CRUST; SURFACE; ORIGIN; EVOLUTION; VOLCANISM; GEOCHEMISTRY; PETROGENESIS; CONSTRAINTS;
D O I
10.1016/j.pss.2008.12.006
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The UK-built Chandrayaan-1 X-ray Spectrometer (C1XS) will fly as an ESA instrument on India's Chandrayaan-1 mission to the Moon, launched in October 2008. C1XS builds on experience gained with the earlier D-C1XS instrument on SMART-1, but will be a scientifically Much more capable instrument. Here we describe the scientific objectives of this instrument, which include mapping the abundances of the major rock-forming elements (principally Mg, Al, Si, Ti, Ca and Fe) in the lunar crust. These data will aid in determining whether regional compositional differences (e.g., the Mg/Fe ratio) are consistent with models Of lunar crustal evolution. C1XS data will also permit geochemical studies of smaller scale features, Such as the ejecta blankets and central peaks of large impact craters, and individual lava flows and pyroclastic deposits. These objectives all bear on important, and currently unresolved, questions in lunar science, including the structure and evolution of any primordial magma ocean, as revealed by vertical and lateral geochemical variations in the crust, and the composition of the lunar mantle, which will further constrain theories of the Moon's origin, thermal history and internal structure. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:725 / 734
页数:10
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