Vendeur : PBShop.store US, Wood Dale, IL, Etats-Unis
PAP. Etat : New. New Book. Shipped from UK. THIS BOOK IS PRINTED ON DEMAND. Established seller since 2000. N° de réf. du vendeur L0-9786209668333
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Vendeur : California Books, Miami, FL, Etats-Unis
Etat : New. N° de réf. du vendeur I-9786209668333
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Vendeur : PBShop.store UK, Fairford, GLOS, Royaume-Uni
PAP. Etat : New. New Book. Delivered from our UK warehouse in 4 to 14 business days. THIS BOOK IS PRINTED ON DEMAND. Established seller since 2000. N° de réf. du vendeur L0-9786209668333
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Vendeur : Grand Eagle Retail, Bensenville, IL, Etats-Unis
Paperback. Etat : 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. N° de réf. du vendeur 9786209668333
Quantité disponible : 1 disponible(s)
Vendeur : BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, Allemagne
Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware 76 pp. Englisch. N° de réf. du vendeur 9786209668333
Quantité disponible : 2 disponible(s)
Vendeur : AussieBookSeller, Truganina, VIC, Australie
Paperback. Etat : 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. N° de réf. du vendeur 9786209668333
Quantité disponible : 1 disponible(s)
Vendeur : Majestic Books, Hounslow, Royaume-Uni
Etat : New. Print on Demand. N° de réf. du vendeur 408468175
Quantité disponible : 4 disponible(s)
Vendeur : Books Puddle, New York, NY, Etats-Unis
Etat : New. N° de réf. du vendeur 26405734672
Quantité disponible : 4 disponible(s)
Vendeur : Biblios, Frankfurt am main, HESSE, Allemagne
Etat : New. PRINT ON DEMAND. N° de réf. du vendeur 18405734682
Quantité disponible : 4 disponible(s)
Vendeur : CitiRetail, Stevenage, Royaume-Uni
Paperback. Etat : 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. N° de réf. du vendeur 9786209668333
Quantité disponible : 1 disponible(s)