Fehlerabschätzung bei Schwermineralanalysen

Barbara Wypyrsczyk, Wolfgang Boenigk & Georg Heumüller
Heavy mineral analysis of pleistocene, pliocene and oligocene Middle Rhine sediments were statistically evaluated in order to identify different Middle Rhine sedimentary cycles and to classify sediments stratigraphically. The scale of deviation in analysis data was determined, treating the facies differentiation of a gravel pit as statistic deviation in a homogeneous embankment.