The large Novoignatievien dyke of andesite porphyrites as an indicator for the fault-block tectonics and the deep structure for the Donbas and Near-Azovian junction zone
DOI:
https://doi.org/10.15407/dopovidi2014.05.110Keywords:
Donbas, indicator, junction zone, Near-Azovian, Novoignatievien dyke, tectonicsAbstract
The large dyke of andesite porphyrites as an indicator of the fault-block tectonics and the deep structure of the Donbas and Near-Azovian junction zone has been studied. The structural geological position of the Novoignatievien dyke, its features, and the conformity with the fault intersection node for the orthogonal and diagonal systems are defined. The possible depths of andesite magma formation are considered.
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