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Friday, December 4, 2020 | History

2 edition of Silica in sediments found in the catalog.

Silica in sediments

Symposium on Silica in Sediments, Los Angeles 1958

Silica in sediments

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Published by Society of Economic Paleontologists and Mineralogists in Tulsa, Okla .
Written in English

    Subjects:
  • Rocks -- Analysis.,
  • Silica.

  • Edition Notes

    SeriesSpecial publication (Society of Economic Paleontologists and Mineralogists) -- no. 7
    ContributionsIreland, Hubert Andrew, 1908-,
    Classifications
    LC ClassificationsQE438 S9 1958
    The Physical Object
    Pagination185p.
    Number of Pages185
    ID Numbers
    Open LibraryOL16720791M


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Silica in sediments by Symposium on Silica in Sediments, Los Angeles 1958 Download PDF EPUB FB2

The Symposium on Silica in Sediments was presented in March, at the meeting in Los Angeles. The subject was selected by the Research Committee and approval of the Council then proceeded to develop the symposium and organized the papers, and later was authorized to edit and prepare the papers for publication.

Silica occurs as amorphous to crystalline form in many types of igneous, metamorphic, and sedimentary rocks, but in sediments and sedimentary rocks much of the silica is detrital material. The chief forms of silica are hydrous opal, crytocrystalline chalcedony, and crystalline quartz.

: Silica in Sediments: Nodular and Bedded Chert (): Earl McBride: BooksAuthor: Earl McBride. OCLC Number: Description: v, pages illustrations, maps (1 folded), diagrams, tables 25 cm. Contents: Introduction to silica in sediments / H. Andrew Ireland --The geochemistry of silica in sedimentary environments / Konrad B.

Krauskopf --The removal of soluble silica from fresh water entering the sea / George S. Bien, David E. Contois and William H. Thomas --The behavior of silica. It has been suggested by some authors that the high silica content of some of the cherts and novaculites is an epigenetic feature resulting from a combination of surface exposure and from alteration of originally non-cherty sediments during the orogeny in which the Ouachita geosyncline was compressed, deformed, and .