THICKNESS OF DENUDATED ROCKS IN THE NORTHEAST OF THE SIBERIAN PLATFORM AND THE KHARAULAKH SEGMENT OF THE VERKHOYANSK FOLDER-THRUST BELT ACCORDING TO LOW-TEMPERATURE GEOCHRONOLOGY

Using low-temperature geochronology methods, the thickness of eroded rocks in the northeast of the Siberian Platform and adjacent areas of the northern front of the Verkhoyansk fold-and-thrust belt was calculated. It has been established that the thickness of eroded rocks increases in the eastern and northern direction from 2-3.3 km in the Lena-Anabar and Priverkhoyansk basins to 6 km in the east in the Central Kharaulakh synclinorium and the Bykov anticlinorium.