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Structural analysis of interior layered deposits in north and south Coprates Chasma, Mars

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dc.contributor.author Racher, Heather
dc.date.accessioned 2011-03-08T18:55:19Z
dc.date.available 2011-03-08T18:55:19Z
dc.date.issued 2011-03-08
dc.identifier.uri http://hdl.handle.net/10464/3181
dc.description.abstract Interior layered deposits within an embayment in the northern as well as near the southern wall of Coprates Chasma in the Valles Marineris, Mars are studied using HRSC, CTX, HiRISE and CRISM data. In the northern embayment, layered deposits outcrop in three separate locations (a western deposit, a central deposit and an eastern deposit). The central layered deposit in the north has a stratigraphic thickness of 2 km. The western layered deposit abuts against the chasma wall appearing to have a relatively un-eroded depositional surface. The eastern deposit is near a landslide scar which appears to have exposed basement layering showing downward displacement. This northern embayment is suggested to have been an ancestral basin. The triangular edged deposit near the southern wall of Coprates Chasma has an elongated mound protruding from the central edge and is suggested to be the outer limits of a fault block which is back rotated 6° south. The rotation may be the result of the Valles Marineris opening. en_US
dc.language.iso eng en_US
dc.publisher Brock University en_US
dc.subject Mars (Planet) en_US
dc.subject Geology -- Mars (Planet) en_US
dc.title Structural analysis of interior layered deposits in north and south Coprates Chasma, Mars en_US
dc.type Electronic Thesis or Dissertation en_US
dc.degree.name M.Sc. Earth Sciences en_US
dc.degree.level Masters en_US
dc.contributor.department Department of Earth Sciences en_US
dc.degree.discipline Faculty of Mathematics and Science en_US


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