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Ancient Impact and Aqueous Processes at Endeavour Crater, Mars

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dc.contributor.author Squyres, S. W.
dc.contributor.author Arvidson, R. E.
dc.contributor.author Bell, J. F.
dc.contributor.author Calef, F.
dc.contributor.author Clark, B. C.
dc.contributor.author Cohen, B. A.
dc.contributor.author Crumpler, L. A.
dc.contributor.author De Souza, P. A.
dc.contributor.author Farrand, W. H.
dc.contributor.author Gellert, R.
dc.contributor.author Grant, John A.
dc.contributor.author Herkenhoff, K. E.
dc.contributor.author Hurowitz, J. A.
dc.contributor.author Johnson, J. R.
dc.contributor.author Jolliff, B. L.
dc.contributor.author Knoll, A. H.
dc.contributor.author Li, R.
dc.contributor.author McLennan, S. M.
dc.contributor.author Ming, D. W.
dc.contributor.author Mittlefehldt, D. W.
dc.contributor.author Parker, T. J.
dc.contributor.author Paulsen, G.
dc.contributor.author Rice, M. S.
dc.contributor.author Ruff, S. W.
dc.contributor.author Schröder, C.
dc.contributor.author Yen, A. S.
dc.contributor.author Zacny, K.
dc.date.accessioned 2012-07-09T14:23:56Z
dc.date.available 2012-07-09T14:23:56Z
dc.date.issued 2012
dc.identifier 0036-8075
dc.identifier.citation Squyres, S. W., Arvidson, R. E., Bell, J. F., Calef, F., Clark, B. C., Cohen, B. A., Crumpler, L. A., de Souza, P. A., Farrand, W. H., Gellert, R., Grant, John A., Herkenhoff, K. E., Hurowitz, J. A., Johnson, J. R., Jolliff, B. L., Knoll, A. H., Li, R., McLennan, S. M., Ming, D. W., Mittlefehldt, D. W., Parker, T. J., Paulsen, G., Rice, M. S., Ruff, S. W., Schröder, C. et al. 2012. "<a href="https://repository.si.edu/handle/10088/18608">Ancient Impact and Aqueous Processes at Endeavour Crater, Mars</a>." <em>Science</em>, 336, (6081) 570–576. <a href="https://doi.org/10.1126/science.1220476">https://doi.org/10.1126/science.1220476</a>.
dc.identifier.issn 0036-8075
dc.identifier.uri http://hdl.handle.net/10088/18608
dc.description.abstract The rover Opportunity has investigated the rim of Endeavour Crater, a large ancient impact crater on Mars. Basaltic breccias produced by the impact form the rim deposits, with stratigraphy similar to that observed at similar-sized craters on Earth. Highly localized zinc enrichments in some breccia materials suggest hydrothermal alteration of rim deposits. Gypsum-rich veins cut sedimentary rocks adjacent to the crater rim. The gypsum was precipitated from low-temperature aqueous fluids flowing upward from the ancient materials of the rim, leading temporarily to potentially habitable conditions and providing some of the waters involved in formation of the ubiquitous sulfate-rich sandstones of the Meridiani region.
dc.format.extent 570–576
dc.relation.ispartof Science 336 (6081)
dc.title Ancient Impact and Aqueous Processes at Endeavour Crater, Mars
dc.type article
sro.identifier.refworksID 85937
sro.identifier.itemID 111385
sro.description.unit NASM-CEPS
sro.description.unit NASM
sro.identifier.doi 10.1126/science.1220476
sro.identifier.url https://repository.si.edu/handle/10088/18608


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