structures induced by liquefaction in Late Pleistocene lacustrine terrace deposits on the
southern shore of Issyk-Kul Lake in the northern Tien Shan mountains of Kyrgyzstan. The
section contains seven deformed beds grouped in two intervals. Five deformed beds in the
upper interval contain load structures (load casts and flame structures), convolute
lamination, ball-and-pillow structures, folds and slumps. Deformation patterns indicate that a …