Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/17069
Appears in Collections:Biological and Environmental Sciences Journal Articles
Peer Review Status: Refereed
Title: Ancient Impact and Aqueous Processes at Endeavour Crater, Mars
Author(s): Squyres, Steven W
Arvidson, Raymond E
Bell III, James F
Calef III, Fred J
Cohen, Barbara A
Clark, Benton C
Crumpler, Larry S
Farrand, William H
Gellert, Ralf
Grant, John A
Herkenhoff, Kenneth E
Hurowitz, Joel A
Johnson, Jeffrey R
Schröder, Christian
Contact Email: christian.schroeder@stir.ac.uk
Issue Date: 4-May-2012
Date Deposited: 23-Oct-2013
Citation: Squyres SW, Arvidson RE, Bell III JF, Calef III FJ, Cohen BA, Clark BC, Crumpler LS, Farrand WH, Gellert R, Grant JA, Herkenhoff KE, Hurowitz JA, Johnson JR & Schröder C (2012) Ancient Impact and Aqueous Processes at Endeavour Crater, Mars. Science, 336 (6081), pp. 570-576. https://doi.org/10.1126/science.1220476
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.
DOI Link: 10.1126/science.1220476
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Notes: Additional co-authors: BL Jolliff, AH Knoll, R Li, SM McLennan, DW Ming, DW Mittlefehldt, TJ Parker, G Paulsen, MS Rice, SW Ruff, AS Yen, K Zacny
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