Potential martian mineral resources: Mechanisms and terrestrial analogues

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Title: Potential martian mineral resources: Mechanisms and terrestrial analogues
Authors: West, Michael D.1,2 michael.west@anu.edu.au, Clarke, Jonathan D.A.3,4 jon.clarke@bigpond.com.au
Source: Planetary & Space Science. Mar2010, Vol. 58 Issue 4, p574-582. 9p.
Subjects: Volcanic activity prediction, Mars surface samples, Hydrothermal deposits, Biomineralization, Impact craters, Ores, Earth analogs to Martian geology, Martian exploration, Martian surface, Mars (Planet)
Abstract: Abstract: The future exploration of Mars is likely to utilize resources that can be extracted in situ. An overview of the geology of Mars has been presented and several mechanisms that could result in the formation of ore deposits have been identified. These include deposits caused by hydrothermal fluids resulting from volcanic activity, large igneous province formation and impact craters. Surface enrichment of mineral sand deposits is also discussed. Where appropriate, terrestrial analogues of these mechanisms have been discussed and supporting evidence from observations of Mars undertaken to date presented. Types of deposits that are unlikely to be found on Mars are also listed. [Copyright &y& Elsevier]
Copyright of Planetary & Space Science is the property of Pergamon Press - An Imprint of Elsevier Science and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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An: 48148342
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  Data: Potential martian mineral resources: Mechanisms and terrestrial analogues
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  Data: <searchLink fieldCode="AR" term="%22West%2C+Michael+D%2E%22">West, Michael D.</searchLink><relatesTo>1,2</relatesTo><i> michael.west@anu.edu.au</i><br /><searchLink fieldCode="AR" term="%22Clarke%2C+Jonathan+D%2EA%2E%22">Clarke, Jonathan D.A.</searchLink><relatesTo>3,4</relatesTo><i> jon.clarke@bigpond.com.au</i>
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  Data: <searchLink fieldCode="JN" term="%22Planetary+%26+Space+Science%22">Planetary & Space Science</searchLink>. Mar2010, Vol. 58 Issue 4, p574-582. 9p.
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  Data: <searchLink fieldCode="DE" term="%22Volcanic+activity+prediction%22">Volcanic activity prediction</searchLink><br /><searchLink fieldCode="DE" term="%22Mars+surface+samples%22">Mars surface samples</searchLink><br /><searchLink fieldCode="DE" term="%22Hydrothermal+deposits%22">Hydrothermal deposits</searchLink><br /><searchLink fieldCode="DE" term="%22Biomineralization%22">Biomineralization</searchLink><br /><searchLink fieldCode="DE" term="%22Impact+craters%22">Impact craters</searchLink><br /><searchLink fieldCode="DE" term="%22Ores%22">Ores</searchLink><br /><searchLink fieldCode="DE" term="%22Earth+analogs+to+Martian+geology%22">Earth analogs to Martian geology</searchLink><br /><searchLink fieldCode="DE" term="%22Martian+exploration%22">Martian exploration</searchLink><br /><searchLink fieldCode="DE" term="%22Martian+surface%22">Martian surface</searchLink><br /><searchLink fieldCode="DE" term="%22Mars+%28Planet%29%22">Mars (Planet)</searchLink>
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  Label: Abstract
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  Data: Abstract: The future exploration of Mars is likely to utilize resources that can be extracted in situ. An overview of the geology of Mars has been presented and several mechanisms that could result in the formation of ore deposits have been identified. These include deposits caused by hydrothermal fluids resulting from volcanic activity, large igneous province formation and impact craters. Surface enrichment of mineral sand deposits is also discussed. Where appropriate, terrestrial analogues of these mechanisms have been discussed and supporting evidence from observations of Mars undertaken to date presented. Types of deposits that are unlikely to be found on Mars are also listed. [Copyright &y& Elsevier]
– Name: AbstractSuppliedCopyright
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  Group: Ab
  Data: <i>Copyright of Planetary & Space Science is the property of Pergamon Press - An Imprint of Elsevier Science and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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      – Type: doi
        Value: 10.1016/j.pss.2009.06.007
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      – Code: eng
        Text: English
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        PageCount: 9
        StartPage: 574
    Subjects:
      – SubjectFull: Volcanic activity prediction
        Type: general
      – SubjectFull: Mars surface samples
        Type: general
      – SubjectFull: Hydrothermal deposits
        Type: general
      – SubjectFull: Biomineralization
        Type: general
      – SubjectFull: Impact craters
        Type: general
      – SubjectFull: Ores
        Type: general
      – SubjectFull: Earth analogs to Martian geology
        Type: general
      – SubjectFull: Martian exploration
        Type: general
      – SubjectFull: Martian surface
        Type: general
      – SubjectFull: Mars (Planet)
        Type: general
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      – TitleFull: Potential martian mineral resources: Mechanisms and terrestrial analogues
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            NameFull: West, Michael D.
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            NameFull: Clarke, Jonathan D.A.
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              Text: Mar2010
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              Y: 2010
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