“…KI is especially useful in reconstructing structural and metamorphic history in very low-to low-grade pelitic rocks (e.g., Frey et al, 1980;Roberts and Merriman, 1985;Frey, 1988;Roberts et al, 1996;Warr et al, 1996;Lee and Ko, 1997). Also, the spatial variation in sediment thickness (e.g., Awan and Woodcock, 1991) and the existence of concealed plutons (e.g., Roberts et al, 1990) can be examined on the basis of KI variation. In this study, KI was used to reconstruct an early history of sedimentary basin development by detecting a major fault related to the initiation of basin formation.…”