The area of study is located in the northern part of the Kharaulakh segment (anticlinorium) of the West-Verkhoyansk sector of the Verkhoyansk fold-thrust belt, which is a deformed passive margin of the Siberian paleocontinent. The Upper Paleozoic and Triassic deposits are represented here by interbedded sandstones, aleurolites and shales, and this is the area of development of the terrigenous Verkhoyansk complex. The structure of the region was considered in a number of papers, but the change in the kinematic characteristics of faults in the reversal zone of regional structures was not discussed in detail. The main objective of this study was to study the structure and reconstruction of stress fields for the reconstruction of the structural evolution of the northern part of the Kharaulakh anticlinorium.
Петрология магматических и метаморфических комплексов : материалы X Всероссийской конференции с международным участием, 27 ноября - 30 ноября 2018 года. Томск, 2018. Вып. 10. С. 277-281