title: Газоносность угленосных массивов Горного Крыма - как один из критериев газоносности шельфа черного моря
abstract: During all stages of tectogenesis it is marked a contingence between tectoni-magmatic events and lithoand sedimentogenesis in time and space. The coal deposits and manifestations in the Mountainous Crimea are attributed to the zones of structural conjugation and areas impacted by tectoni-magmatic processes. Continuation of land structures towards the Black sea shelf gives the chance to predict offshore hydrocarbon accumulations. Coal gas composition indicators from the Beshui suite have been stu
journal: Перший Незалежний Науковий Вісник