ГЕОДИНАМІЧНІ АСПЕКТИ ВУГІЛЬНО-ВУГЛЕВОДНЕВИХ ФОРМАЦІЙ
The sedimentation is only indirectly related to the geodynamic processes generated by the lateral interaction of the lithospheric plates and their displacement, and methods of sedimentary geology objectively tend to represent the primacy of the vertical component of tectonic movements. The urgency o...
Збережено в:
| Дата: | 2018 |
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| Автор: | |
| Формат: | Стаття |
| Мова: | Ukrainian |
| Опубліковано: |
Institute of Geological Sciences of the Ukrainian National Academy of Sciences
2018
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| Теми: | |
| Онлайн доступ: | http://ts.igs-nas.org.ua/article/view/169990 |
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| Назва журналу: | Tectonics and stratigraphy |
Репозитарії
Tectonics and stratigraphy| Резюме: | The sedimentation is only indirectly related to the geodynamic processes generated by the lateral interaction of the lithospheric plates and their displacement, and methods of sedimentary geology objectively tend to represent the primacy of the vertical component of tectonic movements. The urgency of special efforts to solve the problem of coal-hydrocarbon formations is due to a number of reasons. First, the most expressive in the doctrine of carbonaceous formations and their connection with the geosynclinal basis already violates the relations with other sections of geology, which are rapidly modernizing, and hinders the further development of the theory of coal gas formation, as part of a single process of evolution by the Pharrose of the lithosphere. Second, the industrial significance of coal-hydrocarbon formations, which are associated with the resources of the natural energy carrier, valuable technological raw materials, as well as the complex of related coal and hydrocarbons, metallic and non-metallic minerals, requires the prompt involvement of geodynamic analysis in solving the practical problems of coal geology. On the basis of the mobilist theory - tectonics of plates - considered possible reconstruction and with the help of the ordered spatial position synchronous geological complexes, which were formed in typical geodynamic conditions, naturally associated with each other in the system of ancient plates. In combination of the interpretations of the vertical formation series of individual geostructural zones from the positions of the geosynclinal-orogenic cycle and the transition to the predominant lateral geological complexes, developed on large territories, and the peculiarity of the geodynamic aspect of coal-hydrocarbon formations. |
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