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Differential cement mineralogy is influenced by depositional textures, structural deformation, pore fluid chemistry, and ultimately influences landscape evolution by introducing heterogeneities in erodibility. In Southern Utah, the region West of the Kaibab uplift known as Mollies Nipple (Mollies) in Grand Staircase‐Escalante National Monument exhibits a complex history of fluid–sediment interactions,...
Analysis of the history of fluid flow and diagenesis in sandstone deposits can potentially furnish insight into how these deposits function as reservoirs. Imaging spectroscopy provides a way to examine surface mineralogy in order to better understand how this mineralogy might have resulted from past fluid flow and diagenesis. Aerially-acquired spectral data, along with spectral data from field samples,...
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