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sedimentary deposit

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inglês
The lower fluviatile stage consisting of 200250 m thick granular sediment is overlain by lacustrine sedimentary stage of 200-300m section of clay sediment.
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The sedimentary facies in which these fossils were found indicates that ambulocetids inhabited a shallow, swampy near-shore marine environment.
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These form linear belts of mafic, ultramafic and felsic volcanics, intercalated with sedimentary sequences, and have been deformed and metamorphosed.
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The massive beds of sand have hardened to become an extremely weather-resistant sedimentary rock that is some two thousand metres thick in places.
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Grains of sedimentary rock were too large to preserve soft tissues or small and delicate bones.
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This results in development of herringbone sedimentary structures because of the constant differing flow of waves.
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The overall structure of the field is a faulted homocline, with all the sedimentary units dipping in the same direction with little folding.
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Coastal erosion may be the result of sea level rise or deficit in sedimentary equilibrium.
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Cores indicate variations of climate, species and sedimentary composition during geologic history.
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It occurs naturally as the mineral carpathite, which is characterized by flakes of pure coronene embedded in sedimentary rock.
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