The Opportunity Rover's Athena science investigation at Meridiani Planum, Mars.

نویسندگان

  • S W Squyres
  • R E Arvidson
  • J F Bell
  • J Brückner
  • N A Cabrol
  • W Calvin
  • M H Carr
  • P R Christensen
  • B C Clark
  • L Crumpler
  • D J Des Marais
  • C d'Uston
  • T Economou
  • J Farmer
  • W Farrand
  • W Folkner
  • M Golombek
  • S Gorevan
  • J A Grant
  • R Greeley
  • J Grotzinger
  • L Haskin
  • K E Herkenhoff
  • S Hviid
  • J Johnson
  • G Klingelhöfer
  • A H Knoll
  • G Landis
  • M Lemmon
  • R Li
  • M B Madsen
  • M C Malin
  • S M McLennan
  • H Y McSween
  • D W Ming
  • J Moersch
  • R V Morris
  • T Parker
  • J W Rice
  • L Richter
  • R Rieder
  • M Sims
  • M Smith
  • P Smith
  • L A Soderblom
  • R Sullivan
  • H Wänke
  • T Wdowiak
  • M Wolff
  • A Yen
چکیده

The Mars Exploration Rover Opportunity has investigated the landing site in Eagle crater and the nearby plains within Meridiani Planum. The soils consist of fine-grained basaltic sand and a surface lag of hematite-rich spherules, spherule fragments, and other granules. Wind ripples are common. Underlying the thin soil layer, and exposed within small impact craters and troughs, are flat-lying sedimentary rocks. These rocks are finely laminated, are rich in sulfur, and contain abundant sulfate salts. Small-scale cross-lamination in some locations provides evidence for deposition in flowing liquid water. We interpret the rocks to be a mixture of chemical and siliciclastic sediments formed by episodic inundation by shallow surface water, followed by evaporation, exposure, and desiccation. Hematite-rich spherules are embedded in the rock and eroding from them. We interpret these spherules to be concretions formed by postdepositional diagenesis, again involving liquid water.

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عنوان ژورنال:
  • Science

دوره 306 5702  شماره 

صفحات  -

تاریخ انتشار 2004