Correction: Bernardi et al. OH-Defects in Detrital Quartz Grains from the Julian Basin (NE Italy and Slovenia): A Fourier Transform Infrared Study. Geosciences 2022, 12 , 90.

Within the peridotitic spinels, there is a widespread distribution for JB1 and JB17, while they are concentrated within the 50-70 Cr# interval for the two Eocene samples (JB23 and JB26). These parameters show that, for samples JB1, JB23, and JB26, more than 60% of the Cr-spinels are peridotitic, while in JB16 (stratigraphically close to JB17 studied here), they represent only 40% of the Cr spinels (Figure 2c). [Extracted from the article]