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Тhe paper represents the large dyke of andesite porphyrites as an indicator of fault-block tectonics and the deep structure of Donbas and Near-Azovian junction zone has been studied. The structural and geological position of Novoignatievien dyke, its features, and conformity with the fault intersection node for the orthogonal and diagonal systems are defined. The possible depths of andesite magma formation are considered.

THE NOVOIHNATIEVIAN DYKE OF ANDESITE PORPHYRITES FOR THE DONBAS AND NEAR-AZOVIAN JUNCTION ZONE: TECTONICS AND PETROLOGY