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Cerium in chert as an indication of marine environment of its formation HIROSHI SHIMIZU & AKIMASA MASUDA
Department of Earth Sciences, Kobe University, Kobe 657, Japan
THERE are few if any investigations of deep-sea cherts or siliceous sediments from the geochemical point of view, although several geological and mineralogical studies have been published1−6. We present here data on rare-earth elements (REE) in deep-sea cherts, and compare them with relevant data on seawaters as well as cherts exposed on land.
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