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siliceous sediment

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siliceous sediment [sə′lish·əs ′sed·ə·mənt]
(geology)
Fine-grained sediment and sedimentary rock mainly composed of the microscopic remains of the unicellular, silica-secreting plankton diatoms and radiolarians. Minor constituents include extremely small shards of sponge spicules and other microorganisms such as silicoflagellates. Siliceous sedimentary rock sequences are often highly porous and can form excellent petroleum source and reservoir rocks.


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The blue-band color reflectance shows similar cycles, probably because in this band calcite is more reflective than biogenic silica (although both calcareous and siliceous sediments appear white to the human eye).
Underlying the Sheridan Property is a folded sequence of mafic volcanics, subvolcanic gabbro intrusions, siliceous sediments and extensive banded iron formation.
The RC drilling revealed the presence of multiple and structurally complex gold-bearing zones contained within an altered sequence of ferruginous and siliceous sediments.
 
 
 
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