2011
DOI: 10.1086/661110
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Morphologic Clues to the Origins of Iron Oxide–Cemented Spheroids, Boxworks, and Pipelike Concretions, Navajo Sandstone of South-Central Utah, U.S.A.

Abstract: JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact support@jstor.org.. The University of Chicago Press is collaborating with JSTOR to digitize, preserve and extend access to The Journal of Geology. A B S T R A C TConcretions cemented by iron oxid… Show more

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Cited by 35 publications
(44 citation statements)
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“…(2) Excess acid is neutralized by dissolution of siderite tending to drive the reaction from left to right. This mechanism of siderite oxidation is very similar to one we proposed for iron-oxide concretions in the Navajo and Dakota Sandstones (Loope et al, , 2011Weber et al, 2012).…”
supporting
confidence: 82%
“…(2) Excess acid is neutralized by dissolution of siderite tending to drive the reaction from left to right. This mechanism of siderite oxidation is very similar to one we proposed for iron-oxide concretions in the Navajo and Dakota Sandstones (Loope et al, , 2011Weber et al, 2012).…”
supporting
confidence: 82%
“…Upon oxidation by contact with another fluid, such as meteoric groundwater, solubilized iron oxide minerals are reprecipitated as porefill cement (Chan et al, 2000Chan and Parry, 2002;Bowen et al, 2007). It is also possible for precursor minerals (e.g., pyrite) to be precipitated early and later oxidized to iron oxide minerals (Dinwiddie et al, 2011;Loope et al, 2011;Chan et al, 2012;Potter-McIntyre et al, 2014).…”
Section: Previous Workmentioning
confidence: 99%
“…This has variously been attributed to bleaching by buoyant hydrocarbons and methane rich brine (Beitler et al, 2003(Beitler et al, , 2005Chan et al, 2000;Garden et al, 2001;Parry et al, 2004Parry et al, , 2009) and by dense CO 2 -charged brine containing methane or sulfide reductants (Loope et al, 2010(Loope et al, , 2011Potter-McIntyre et al, 2013;Wigley et al, 2012, Figure 6. (A) Bleached basal sandstones of the Entrada Sandstone hosting CO 2 charged fluids.…”
Section: Co2w55 Core Stratigraphymentioning
confidence: 99%