9786209668333 - Problems of halogenesis: Experience in developing a new concept de Kislík, Valeryan (13 resultados)

Condición: New.

Condición: New.

Taschenbuch. Condición: Neu. Problems of halogenesis | Experience in developing a new concept | Valeryan Kislík | Taschenbuch | Englisch | 2026 | Our Knowledge Publishing | EAN 9786209668333 | Verantwortliche Person für die EU: SIA OmniScriptum Publishing, Brivibas Gatve 197, 1039 RIGA, LETTLAND, customerservice[at]vdm-vsg[dot]de | Anbieter: preigu.

PAP. Condición: New. New Book. Shipped from UK. THIS BOOK IS PRINTED ON DEMAND. Established seller since 2000.

PAP. Condición: New. New Book. Delivered from our UK warehouse in 4 to 14 business days. THIS BOOK IS PRINTED ON DEMAND. Established seller since 2000.

Paperback. Condición: new. Paperback. The evolution of the world's oceans is moving from chloride to hydrocarbonate and from essentially juvenile to essentially vadose. The megacycles of halogenesis are determined by the state of thermodynamic activity in the subsurface, which ultimately manifests itself in the release of energy into sedimentation basins. Specific phases of halogenesis reflect the moment of introduction of chlorine-calcium waters into the marine basin. To understand the processes of halogenesis, it is essential to identify the links between the conditions for the formation of powerful salt-bearing formations and global geological processes. When assessing the evolution of salt formation in the Neogene, the role of geochemical evolution in the history of the Earth and the development of lithogenesis processes in connection with changes in the composition of the atmosphere and hydrosphere is emphasized. Rift zones (such as the Pripyat Rift) and the deep faults that form them are structures that contribute to the release of energy from the subsurface with the release of degassing products into sedimentary basins. A genetic link is noted between the appearance of oceans on Earth, the formation of their water composition, salt-bearing basins, replacement zones in potash horizons, and salt dome structures. This item is printed on demand. Shipping may be from multiple locations in the US or from the UK, depending on stock availability.

Taschenbuch. Condición: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware 76 pp. Englisch.

Condición: New. Print on Demand.

Paperback. Condición: new. Paperback. The evolution of the world's oceans is moving from chloride to hydrocarbonate and from essentially juvenile to essentially vadose. The megacycles of halogenesis are determined by the state of thermodynamic activity in the subsurface, which ultimately manifests itself in the release of energy into sedimentation basins. Specific phases of halogenesis reflect the moment of introduction of chlorine-calcium waters into the marine basin. To understand the processes of halogenesis, it is essential to identify the links between the conditions for the formation of powerful salt-bearing formations and global geological processes. When assessing the evolution of salt formation in the Neogene, the role of geochemical evolution in the history of the Earth and the development of lithogenesis processes in connection with changes in the composition of the atmosphere and hydrosphere is emphasized. Rift zones (such as the Pripyat Rift) and the deep faults that form them are structures that contribute to the release of energy from the subsurface with the release of degassing products into sedimentary basins. A genetic link is noted between the appearance of oceans on Earth, the formation of their water composition, salt-bearing basins, replacement zones in potash horizons, and salt dome structures. This item is printed on demand. Shipping may be from our Sydney, NSW warehouse or from our UK or US warehouse, depending on stock availability.

Paperback. Condición: new. Paperback. The evolution of the world's oceans is moving from chloride to hydrocarbonate and from essentially juvenile to essentially vadose. The megacycles of halogenesis are determined by the state of thermodynamic activity in the subsurface, which ultimately manifests itself in the release of energy into sedimentation basins. Specific phases of halogenesis reflect the moment of introduction of chlorine-calcium waters into the marine basin. To understand the processes of halogenesis, it is essential to identify the links between the conditions for the formation of powerful salt-bearing formations and global geological processes. When assessing the evolution of salt formation in the Neogene, the role of geochemical evolution in the history of the Earth and the development of lithogenesis processes in connection with changes in the composition of the atmosphere and hydrosphere is emphasized. Rift zones (such as the Pripyat Rift) and the deep faults that form them are structures that contribute to the release of energy from the subsurface with the release of degassing products into sedimentary basins. A genetic link is noted between the appearance of oceans on Earth, the formation of their water composition, salt-bearing basins, replacement zones in potash horizons, and salt dome structures. This item is printed on demand. Shipping may be from our UK warehouse or from our Australian or US warehouses, depending on stock availability.

Condición: New. PRINT ON DEMAND.

Taschenbuch. Condición: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The evolution of the world's oceans is moving from chloride to hydrocarbonate and from essentially juvenile to essentially vadose. The megacycles of halogenesis are determined by the state of thermodynamic activity in the subsurface, which ultimately manifests itself in the release of energy into sedimentation basins. Specific phases of halogenesis reflect the moment of introduction of chlorine-calcium waters into the marine basin. To understand the processes of halogenesis, it is essential to identify the links between the conditions for the formation of powerful salt-bearing formations and global geological processes. When assessing the evolution of salt formation in the Neogene, the role of geochemical evolution in the history of the Earth and the development of lithogenesis processes in connection with changes in the composition of the atmosphere and hydrosphere is emphasized. Rift zones (such as the Pripyat Rift) and the deep faults that form them are structures that contribute to the release of energy from the subsurface with the release of degassing products into sedimentary basins. A genetic link is noted between the appearance of oceans on Earth, the formation of their water composition, salt-bearing basins, replacement zones in potash horizons, and salt dome structures.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 76 pp. Englisch.

Taschenbuch. Condición: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering.