Digital topographic analysis and lineament interpretation south of the Lena Delta, North Siberia: Landscape expression of its tectonic activity

• Main Authors: Hamann, Jakob S., Baranskaya, Alisa V., Geissler, Wolfram H., Baranov, Boris V., Tsukanov, Nikolay V.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2024
• Subjects: Tectonic Geomorphology; Lineament Identification; Topographic Analysis; Hypsometry; Arctic Landscapes; ddc:550; Arctic; Kharaulakh; Laptev Sea; Verkhoyansk; laptev; lena delta; Siberia
• Online Access: https://refubium.fu-berlin.de/handle/fub188/44846; https://doi.org/10.17169/refubium-44556; https://doi.org/10.1016/j.geomorph.2024.109228

This study applies semi-automated techniques to analyze the landforms, morphostructure, and geology of the Kharaulakh and Chekanovsky sectors, south of the Lena Delta, northern Siberia. High-resolution data, including TanDEM-X 30 m spatial resolution Digital Elevation Models (DEM), 2 m spatial resolution ArcticDEM Digital Surface Models (DSM), and Sentinel-2 satellite imagery, serve as the basis for the analysis. Digital terrain classification and identification of tectonic lineaments are performed using the Benthic Terrain Modeler (BTM) and Linear Extraction (LINE) algorithm, respectively. Additionally, a hypsometric analysis is conducted to assess areas of potential neotectonic activity. 873 lineaments are identified, primarily in NE-SW and E-W orientations. NW-SE lineaments perpendicular to the lithological and fold belt strikes in the Kharaulakh Ridge suggest inheritance from original depositional settings or later compressional tectonics, now appearing as valleys and weak zones facilitating erosion and river incision. Longer N-S or NNW-SSE lineaments in the Kharaulakh Sector are associated with thrust sheets of the Verkhoyansk fold-and-thrust belt and Cenozoic graben structures linked to the formation of the Laptev Sea Rift System and ongoing regional deformation. The Chekanovsky Sector, marked by epiplatform blocks and hills, presents a dissected plateau with steep valleys. Here, high hypsometric integral values are attributed to compression and uplift near the southwestern boundary of the Laptev Sea Microplate.