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Clays and formation of deep-sea chert (1974)

KEENE, J. B. ; KASTNER, MIRIAM

[s.l.] : Nature Publishing Group

Nature 249 (1974), S. 754-755

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ISSN: 1476-4687

Source: Nature Archives 1869 - 2009

Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics

Notes: [Auszug] Biogenous opal is the principal source of silica for the formation of chert12. Silica may also be produced by the alteration of volcanic detritus, resulting in the mineral assemblage smectite, zeolite and opal3*4. A third possible source, not previously suggested in the literature, is the ...

Type of Medium: Electronic Resource

URL: http://dx.doi.org/10.1038/249754a0

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