2015
DOI: 10.1016/j.jappgeo.2015.05.002
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Resolving electrolayers from VES: A contribution from modeling the electrical response of a tightly constrained alluvial stratigraphy

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Cited by 6 publications
(9 citation statements)
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“…In particular, the results obtained at the key-sectors showed, as a whole, that a hierarchical structure of the EsUs emerges when exploring a sedimentary sequence; this structure is independent of any calibration between each VES and the lito-stratigraphy of a neighbouring 1-D borehole (Mele et al , 2013(Mele et al , 2015.…”
mentioning
confidence: 94%
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“…In particular, the results obtained at the key-sectors showed, as a whole, that a hierarchical structure of the EsUs emerges when exploring a sedimentary sequence; this structure is independent of any calibration between each VES and the lito-stratigraphy of a neighbouring 1-D borehole (Mele et al , 2013(Mele et al , 2015.…”
mentioning
confidence: 94%
“…After a set of studies dedicated to improve and test the detailed resistivity imaging of the Po basin subsurface at the local scale (Bersezio et al 2007;Mele et al , 2013Mele et al , 2015, we now apply this approach to a wide scale casestudy, that is the electrostratigraphy of a regional N-S cross-section across the Quaternary Po foreland basin in Northern Italy, East and South of Milan. The tectono-sedimentary setting of the basin is recorded by alluvial and glacio-fluvial clastic, regressive depositional systems, which prograde above shallow marine sediments, under the control of Pleistocene glacial cycles and Apennine-related tectonics.…”
Section: Introductionmentioning
confidence: 99%
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“…From these data, other textural parameters were calculated: the characteristic diameters d10,d30,d50,d60 and d90 that indicate the grain diameter at 10%, 30%, 50%, 60%, and 90% passing, respectively; the uniformity coefficients U60 and U90, which were calculated as the ratio between d60 and d10 and d90 and d10, respectively, and the curvature coefficient Uc calculated as Uc=d302d10d60; the coarse‐to‐fine ratios Γd with threshold grain diameters d equal to 0.125 and 0.250 mm (Mele, Bersezio, and Giudici ; Mele et al . , ). …”
Section: Methodsmentioning
confidence: 99%
“…• the coarse-to-fine ratios Γ d with threshold grain diameters d equal to 0.125 and 0.250 mm (Mele, Bersezio, and Giudici 2012;Mele et al 2014Mele et al , 2015. Furthermore, the porosity of each sample was estimated from the water content at full saturation.…”
Section: Materials and Methods Sample Characteristicsmentioning
confidence: 99%