The Self-Organization of the Earth's Geological Development

Kirjan The Self-Organization of the Earth's Geological Development (2024) on kirjoittanut Arkadiy Kopylov. Kirjan kieli on englanti, ja sen on kustantanut Lap Lambert Academic Publishing. Kirja on laajuudeltaan 264 sivua ja se on pokkari.

The Earth is regarded as an open non-stationary dynamic physical and chemical system with one common property: the vibration of all its composition, structure and state elements. The structural-material associations synchronous for interval chaos - order from the series: atom - element - ion - molecule - mineral - rock (formational) periodic from composition Solar System in the history of Earth is formed. The variety of dissipative and fractal geological structures - structural-material complexes (SMC) originate at the microscopic level in the process of self-organization of the field of resonances and go through several stages. The formation of the Earth's lithosphere is presented as a periodic a self-similar repeated repetition of structural-material complexes (SMC) for of 4. 5 billion years. Each SMC includes the synchronous igneous (ultra-basic, basic-diorite-granite part), ore, sedimentary, metamorphic, etc. geological formations and related phenomena and structures formed at a certain stage of the Earth's development. The self-organization of the Earth's Crust of the Pamirs (the west of the Himalayas Orogen) is considered.