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Siliciclastic sediments are silica-based sediments, lacking carbon compounds, which are formed from pre-existing rocks, by breakage, transportation and redeposition to form sedimentary rock.
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Cross beds in siliciclastic shoreface sediment (Agadir-Essaouira Basin, Morocco)
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that are composed primarily of silicate minerals, such as
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Type of rocks that are almost exclusively silica-bearing
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53:. Siliciclastic rock types include
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