Примеры использования Limestones на Английском языке и их переводы на Русский язык
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Geological formations recorded are mainly-basaltic volcanic rocks interspersed with tertiary limestones and occasional inter-bedded volcanics overlaid by phosphate-rich soils on the surface in some areas.
specializing in the production of industrial and construction limestones of different fractions, sand, gravel.
It is established that the high porosity of the Carbonate reservoirs of the Turnaian stage is due to the processes of leaching calcite cement from limestones.
Cyclocarcinoides serratus and Mesoprosopon triasinum are found in the grey Norian(late Triassic) limestones of Bad Ischl in the Austrian Salzkammergut.
The article considers the influence of the processes of hypergenesis on the formation of oil deposits in organogenic limestones of the Tournaisian and Bashkirian stages of the Demkinsky oil field.
clay, limestones and other minerals are also found.
Narva River Canyon and waterfall escarpments cut into representative Lower Ordovician limestones.
Dolomitic limestones are common along rivers Vazuza, Osugi, Tsna( marble-like limestone), there are deposits of tile,
Jurassic karstified limestones, strong links to surface water systems,
Jurassic karstic limestones, dolomites, marbles,
Bosnia and herzegovina montenegro Does not correspond to any of the described model aquifer types; Triassic, Jurassic and Cretaceous limestones and dolomites; weakly linked to surface waters;
Jurassic and Cretaceous limestones in large anticlines with flysch in synclines; strong links with surface water systems;
flux limestones, refractories, coke as the main type of fuel,
partly Tertiary carbonates, and karstic limestones; unconfined;
Bosnia and herzegovina Croatia Does not correspond to any of the described model aquifer types(see Figure 1); Triassic, Jurassic, Cretaceous layered and massive limestones, with local Eocene flysch;
Type 4; Upper Jurassic- Lower Cretaceous karstic limestones, dolomites and dolomitic limestones; weak links with surface water systems;
The limestones of Shakhtau are characterized by the usual qualities of limestones of organogenic structures:
Here limestones, clays and sands lie on Precambrian formations- gneisses
and Triassic and Jurassic karstic limestones; minor alluvial sediments with free(unconfined) groundwater; groundwater flow occurs in both directions,
Cretaceous karstic limestones and dolomites; groundwater flow generally from east to west from Bosnia