“…11 Comparison between the obtained frequency-thickness relationships for the Iška alluvial fan and the Ljubljana Moor basin. Parolai et al (2002) Cologne, Germany 108 -1.5510 Hinzen et al (2004) Lower-Rhine East, Germany 137 -1.1900 Garcia-Jerez et al (2006) Zafarraya Basin, Spain 194.6 -1.1400 Motamed et al (2006) Bam, Iran 135.19 -1-9790 Gosar and Lenart (2010) Ljubljana Moor, Slovenia 105.53 -1.2500 Mascandolla et al (2019) Po Plain, Italy 098 -1.1700 Poggi et al (2012) Lucerne, Switzerland 158.54 -2.4500 D' Amico et al (2008) Florence, Italy 140 -1.1720 Birgören et al (2009) Istanbul, Turkey 150.99 -1.1531 Del'Monaco et al (2013) L'Aquila, Italy 053.461 -1.0100 Dinesh et al (2010) Bangalore, India 058.3 -0.9500 Maresca and Berrino (2016) Volturara Irpina, Italy 129 -1.3800 Özalaybey et al (2011) Izmit Bay, Turkey 141 -1.2700 Paudyal et al (2013) Kathmandu Basin, Nepal 146.01 -1.2079 Sukumaran et al (2011) Narmada Valley, India 102.1 -1.4700 Joshi et al (2018) Aravalli, India 056.8 -1.0000 Sant et al (2017) Banni Plains, India 110.18 -1.9700 Liang et al (2018) Pearl River Delta, China 055 -1.0200 Pugin et al (2013) Ottawa, Canada 064. 98 -1.1980 This study Iška alluvial fan, Slovenia 202.97 -1.1390 therefore reveals in general a small variation of b values, and a rather large range of a values, which again implies that the parameter a is characteristic for certain areas.…”