2017
DOI: 10.12681/bgsg.11228
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Sedimentological and Geophysical Observations in the Delta Plain of Selinous River, Ancient Helike, Northern Peloponnesus Greece

Abstract: Fine and coarse grained lithofacies and depositional environments were distinguished in Selinous

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Cited by 4 publications
(3 citation statements)
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“…The average electrical resistivity depth slices from 0-10 m (Figure 8A) and 20-50 m (Figure 8B) suggest that conductive earth materials dominate the uppermost 50 m with resistivities (<80 Ωm) typical of saturated alluvial deposits (Soupios et al [1,2]; Koutsios et al [4]; Kanta et al [5]; Mollidor et al [6]; von Papen et al [7]; Yogeshwar et al [8]; Kourgialas et al [9]). The electrical resistivity depth slice from 0-10 m shows a dominant conductive anomaly with resistivity values <20 Ωm that widens coastwards and is wrapped by slightly less conductive materials (20 to 80 Ωm).…”
Section: Depth Slices Of Average Electrical Resistivitymentioning
confidence: 99%
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“…The average electrical resistivity depth slices from 0-10 m (Figure 8A) and 20-50 m (Figure 8B) suggest that conductive earth materials dominate the uppermost 50 m with resistivities (<80 Ωm) typical of saturated alluvial deposits (Soupios et al [1,2]; Koutsios et al [4]; Kanta et al [5]; Mollidor et al [6]; von Papen et al [7]; Yogeshwar et al [8]; Kourgialas et al [9]). The electrical resistivity depth slice from 0-10 m shows a dominant conductive anomaly with resistivity values <20 Ωm that widens coastwards and is wrapped by slightly less conductive materials (20 to 80 Ωm).…”
Section: Depth Slices Of Average Electrical Resistivitymentioning
confidence: 99%
“…Transient electromagnetic (TEM) surveys have effectively mapped the electrical resistivity structure of various Late Neogene-Quaternary sedimentary basins of distinct depositional environments (Soupios et al [1,2]; Vallianatos [3]; Koutsios et al [4]; Kanta et al [5]; Mollidor et al [6]; von Papen et al [7]; Yogeshwar et al [8]; Kourgialas et al [9]; Autio et al [10]; Demirci et al [11]; Kalisperi et al [12]; Rani et al [13].) TEM data can also be used to correct static shifts in magnetotelluric data surveys (Ruiz-Aguilar et al [14]).…”
Section: Introductionmentioning
confidence: 99%
“…With the accessibility of global remote sensing databases, the physical attributes of deltaic systems are becoming increasingly better quantified [10] , [11] , [12] , [13] , [14] . Geophysical surveys have been conducted in many deltaic regions and coastal zones around the world [15] , [16] , [17] , [18] , [19] , [20] , [21] , [22] .…”
Section: Introductionmentioning
confidence: 99%