High-Temperature, Perhaps Silicic, Volcanism on Mars Evidenced by Tridymite Detection in High-SiO2 Sedimentary Rock at Gale Crater, Mars

نویسندگان

  • R. V. Morris
  • D. T. Vaniman
  • D. F. Blake
  • R. Gellert
  • S. J. Chipera
  • E. B. Rampe
  • D. W. Ming
  • S. M. Morrison
  • R. T. Downs
  • A. H. Treiman
  • A. S. Yen
  • C. N. Achilles
  • T. F. Bristow
  • J. A. Crisp
  • D. J. Des Marais
  • J. D. Farmer
  • K. V. Fendrich
  • J. Frydenvang
  • T. G. Graff
  • J. P. Grotzinger
  • J. M. Morookian
  • S. P. Schwenzer
چکیده

Morris, R. V.; Vaniman, D. T.; Blake, D. F.; Gellert, R.; Chipera, S. J.; Ming, D. W.; Morrison, S. M.; Downs, R. T.; Rampe, E. B.; Treiman, A. H.; Yen, A. S.; Achilles, C. N.; Bristow, T. F.; Fendrich, K.; Crisp, J. A.; Des Marais, D. J. ; Farmer, J. D. ; Grotzinger, J. P.; Morookian, J. M. and Schwenzer, S. P. (2016). High-Temperature, Perhaps Silicic, Volcanism on Mars Evidenced by Tridymite Detection in High-SiO2 Sedimentary Rock at Gale Crater, Mars. In: 47th Lunar and Planetary Science Conference, 21-25 March, 2016, Houston, Texas.

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تاریخ انتشار 2016