Rinded iron-oxide concretions: Hallmarks of altered …
many of the iron-rich concretions are localized at joints (Loope et al., 2010) and the central zones of some concretions contain iron-oxide pseudomorphs after siderite (Loope et al., 2011). These relationships indicate not only that the concretions of the Navajo Sandstone had siderite precursors, but also that these formed during late diagenesis.
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