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Thin-skinned deformation of sedimentary rocks in Valles Marineris, Mars

Metz, Joannah and Grotzinger, John and Okubo, Chris and Milliken, Ralph (2010) Thin-skinned deformation of sedimentary rocks in Valles Marineris, Mars. Journal of Geophysical Research E, 115 . Art. No. E11004. ISSN 0148-0227. https://resolver.caltech.edu/CaltechAUTHORS:20101220-144528706

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Abstract

Deformation of sedimentary rocks is widespread within Valles Marineris, characterized by both plastic and brittle deformation identified in Candor, Melas, and Ius Chasmata. We identified four deformation styles using HiRISE and CTX images: kilometer-scale convolute folds, detached slabs, folded strata, and pull-apart structures. Convolute folds are detached rounded slabs of material with alternating dark- and light-toned strata and a fold wavelength of about 1 km. The detached slabs are isolated rounded blocks of material, but they exhibit only highly localized evidence of stratification. Folded strata are composed of continuously folded layers that are not detached. Pull-apart structures are composed of stratified rock that has broken off into small irregularly shaped pieces showing evidence of brittle deformation. Some areas exhibit multiple styles of deformation and grade from one type of deformation into another. The deformed rocks are observed over thousands of kilometers, are limited to discrete stratigraphic intervals, and occur over a wide range in elevations. All deformation styles appear to be of likely thin-skinned origin. CRISM reflectance spectra show that some of the deformed sediments contain a component of monohydrated and polyhydrated sulfates. Several mechanisms could be responsible for the deformation of sedimentary rocks in Valles Marineris, such as subaerial or subaqueous gravitational slumping or sliding and soft sediment deformation, where the latter could include impact-induced or seismically induced liquefaction. These mechanisms are evaluated based on their expected pattern, scale, and areal extent of deformation. Deformation produced from slow subaerial or subaqueous landsliding and liquefaction is consistent with the deformation observed in Valles Marineris.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1029/2010JE003593DOIArticle
ORCID:
AuthorORCID
Grotzinger, John0000-0001-9324-1257
Milliken, Ralph0000-0003-3240-4918
Additional Information:© 2010 American Geophysical Union. Received 1 March 2010; accepted 3 August 2010; published 19 November 2010. We would like to acknowledge the contributions of the HiRISE science and operations team who made this work possible.
Subject Keywords:Mars; tectonics; Valles Marineris
Record Number:CaltechAUTHORS:20101220-144528706
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20101220-144528706
Official Citation:Metz, J., J. Grotzinger, C. Okubo, and R. Milliken (2010), Thin-skinned deformation of sedimentary rocks in Valles Marineris, Mars, J. Geophys. Res., 115, E11004, doi:10.1029/2010JE003593
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:21454
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:05 Jan 2011 20:03
Last Modified:09 Mar 2020 13:19

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