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Some intra-cratonic basins are traditionally called “aulacogens”. This term   has persisted in the geoscience literature since its invention by Soviet   geologists in the mid-20th century before the triumph of the plate tectonics,   but its meaning has evolved. Attempts to change its meaning from descriptive   to genetic have led to a broad spectrum of opinions on the definition of   aulacogens. Some specialists related them to continental rifts, while others   have restricted aulacogens to the only particular rift systems or peculiar   stages in the evolution of young cratons. The Donets Basin is a typical   aulacogen stretching across the southern margin of the East European Craton.   A brief review of present knowledge of this basin shows that its nature is   rather incompatible with the present understanding of aulacogens. Instead,   the new classification of rifts offers a more precise terminology for its   exact characteristics. It is suggested that the term “aulacogen” should only   be restricted to those basins for which it has been applied historically

Aulacogens, the Donets Basin (Eastern Ukraine, Southwestern Russia), and the new classification of rifts: Towards a proper terminology