Clarification of the position of the Mohorowicz surface: According to retrospective data on nomenclature sheets n-51-53, m-52-54

Data on the deep structure of the territory, in particular, on the depth of the main deep boundaries over the basement, the Conrad and Moho surfaces, are of great importance for studying the distribution patterns of minerals. On the territory of the Far Eastern District, one of the last Moho maps was constructed in 2014 by Shevchenko et al. It was constructed using GSR profiles and does not take into account the data on a number of regional seismic profiles available in the territory. Therefore, there is an opportunity to update the Moho depth map based on all available seismic information.