Space Science Reviews

, Volume 96, Issue 1, pp 317–330

Chemical Composition of Rocks and Soils at the Pathfinder Site

Authors

  • H. Wänke
    • Max-Planck-Institut für Chemie
  • J. Brückner
    • Max-Planck-Institut für Chemie
  • G. Dreibus
    • Max-Planck-Institut für Chemie
  • R. Rieder
    • Max-Planck-Institut für Chemie
  • I. Ryabchikov
    • IGEM, Russian Academy of Sciences
Article

DOI: 10.1023/A:1011961725645

Cite this article as:
Wänke, H., Brückner, J., Dreibus, G. et al. Space Science Reviews (2001) 96: 317. doi:10.1023/A:1011961725645

Abstract

As Viking Landers did not measure rock compositions, Pathfinder (PF) data are the first in this respect. This review gives no proof yet whether the PF rocks are igneous or sedimentary, but for petrogenetic reasons they could be igneous. We suggest a model in which Mars is covered by about 50% basaltic and 50% andesitic igneous rocks. The soils are a mixture of the two with addition of Mg-sulfate and -chloride plus iron compounds possibly derived from the hematite deposits.

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© Kluwer Academic Publishers 2001