Da: PBShop.store US, Wood Dale, IL, U.S.A.
PAP. Condizione: New. New Book. Shipped from UK. THIS BOOK IS PRINTED ON DEMAND. Established seller since 2000. Codice articolo L0-9786209668333
Quantità: Più di 20 disponibili
Da: California Books, Miami, FL, U.S.A.
Condizione: New. Codice articolo I-9786209668333
Quantità: Più di 20 disponibili
Da: PBShop.store UK, Fairford, GLOS, Regno Unito
PAP. Condizione: New. New Book. Delivered from our UK warehouse in 4 to 14 business days. THIS BOOK IS PRINTED ON DEMAND. Established seller since 2000. Codice articolo L0-9786209668333
Quantità: Più di 20 disponibili
Da: Grand Eagle Retail, Bensenville, IL, U.S.A.
Paperback. Condizione: 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. Codice articolo 9786209668333
Quantità: 1 disponibili
Da: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, Germania
Taschenbuch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware 76 pp. Englisch. Codice articolo 9786209668333
Quantità: 2 disponibili
Da: AussieBookSeller, Truganina, VIC, Australia
Paperback. Condizione: 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. Codice articolo 9786209668333
Quantità: 1 disponibili
Da: Majestic Books, Hounslow, Regno Unito
Condizione: New. Print on Demand. Codice articolo 408468175
Quantità: 4 disponibili
Da: Books Puddle, New York, NY, U.S.A.
Condizione: New. Codice articolo 26405734672
Quantità: 4 disponibili
Da: Biblios, Frankfurt am main, HESSE, Germania
Condizione: New. PRINT ON DEMAND. Codice articolo 18405734682
Quantità: 4 disponibili
Da: CitiRetail, Stevenage, Regno Unito
Paperback. Condizione: 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. Codice articolo 9786209668333
Quantità: 1 disponibili