PROBLEMS OF DISPLAYING THE ESSENCE OF GEODYNAMIC PROCESSES ON GEOLOGICAL MAPS

Abstract

Abstract. In connection with the transition to a new paradigm in geology offered by "Lithospheric plate tectonics", it became known that it is difficult to show the geological features of complex dislocated layered structures on geological maps, because the geological significance of such structures is the result of the horizontal movement of matter (geological formations) in time and space and the attributes of these formations in the current erosion section. combination, and the map sheet itself is ultimately a static sheet of paper. This situation requires the development of qualitative new methods and methodology for mapping highly dislocated tectonic structures, a vivid example of which is called "Pre-Late Paleozoic Ophiolitic Zones of Kazakhstan". ", it turns out that it is difficult to display the geological features of complex folded structures on geological maps, since the geological essence of such structures is the result of the horizontal movement of matter (geological formations) in time and space with the subsequent combination of the attributes of these formations on the modern erosion section, while the sheet of the map itself It is, after all, a static sheet of paper. This circumstance requires the development of qualitatively new methods and methodologies for mapping highly dislocated tectonic structures, a striking example of which are the so-called "Late Precambrian-Paleozoic ophiolite zones of Kazakhstan".