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dc.contributor.authorSchröder, C.
dc.contributor.authorBland, Phil
dc.contributor.authorGolombek, M.
dc.contributor.authorAshley, J.
dc.contributor.authorWarner, N.
dc.contributor.authorGrant, J.
dc.date.accessioned2017-01-30T11:00:20Z
dc.date.available2017-01-30T11:00:20Z
dc.date.created2016-12-06T19:30:20Z
dc.date.issued2016
dc.identifier.citationSchröder, C. and Bland, P. and Golombek, M. and Ashley, J. and Warner, N. and Grant, J. 2016. Amazonian chemical weathering rate derived from stony meteorite finds at Meridiani Planum on Mars. Nature Communications. 7 (13459).
dc.identifier.urihttp://hdl.handle.net/20.500.11937/7516
dc.identifier.doi10.1038/ncomms13459
dc.description.abstract

© The Author(s) 2016.Spacecraft exploring Mars such as the Mars Exploration Rovers Spirit and Opportunity, as well as the Mars Science Laboratory or Curiosity rover, have accumulated evidence for wet and habitable conditions on early Mars more than 3 billion years ago. Current conditions, by contrast, are cold, extremely arid and seemingly inhospitable. To evaluate exactly how dry today's environment is, it is important to understand the ongoing current weathering processes. Here we present chemical weathering rates determined for Mars. We use the oxidation of iron in stony meteorites investigated by the Mars Exploration Rover Opportunity at Meridiani Planum. Their maximum exposure age is constrained by the formation of Victoria crater and their minimum age by erosion of the meteorites. The chemical weathering rates thus derived are ~1 to 4 orders of magnitude slower than that of similar meteorites found in Antarctica where the slowest rates are observed on Earth.

dc.publisherMacmillan Publishers Limited
dc.rights.urihttps://creativecommons.org/licenses/by-nc/4.0/
dc.titleAmazonian chemical weathering rate derived from stony meteorite finds at Meridiani Planum on Mars
dc.typeJournal Article
dcterms.source.volume7
dcterms.source.titleNature Communications
curtin.departmentDepartment of Applied Geology
curtin.accessStatusOpen access


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