“…The Oslo method has previously been applied for rare earth nuclei, obtaining information on the level density and average γ-decay properties in this mass region [6,7]. Recently, the method has been extended to other mass regions like Fe, Mo, V and Sc [8,9,10,11,12]. In order to check the validity of the method in cases where nuclei have low level density and strong Porter-Thomas fluctuations [13], the 27,28 Si nuclei were studied with gratifying results [14].…”