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We present the sedimentological survey of Quaternary sediments developed in glacio-fluvial to glacio-lacustrine delta environments and exposed at an abandoned quarry in Northern Italy. This outcrop is considered an analogue of sedimentary structures that could form a real aquifer. We recognise the following sedimentary units: (I) colluvial sediments with human artefacts (less than 2 m thick); (II)...
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