Formation of calcium silicates during ignition of marine sediments and its implication on the state of silica on the sea floor

Details Formation of calcium silicates during ignition of marine sediments and its implication on the state of silica on the sea floor Formation of calcium silicates during ignition of marine sediments and its implication on the state of silica on the sea floor

Jun 1974

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1974gecoa..38..967d&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 38, Issue 6, pp.967-973

Physics

Scientific paper

Anomalies in the formation of calcium silicates in various marine
sediment samples were observed on ignition at 800°C. The hypothesis
is put forward that silica, originating from the land and from marine
diatoms, undergoes a slow hydrolysis in the seabed and becomes more
reactive.

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