Artigo Revisado por pares

Framework mineralogy and chemical composition of continental margin-type sandstone

1975; Geological Society of America; Volume: 3; Issue: 9 Linguagem: Inglês

10.1130/0091-7613(1975)3 2.0.co;2

ISSN

1943-2682

Autores

Frederic L. Schwab,

Tópico(s)

Geological formations and processes

Resumo

Research Article| September 01, 1975 Framework mineralogy and chemical composition of continental margin-type sandstone Frederic L. Schwab Frederic L. Schwab 1Department of Geology, Washington and Lee University, Lexington, Virginia 24450 Search for other works by this author on: GSW Google Scholar Geology (1975) 3 (9): 487–490. https://doi.org/10.1130/0091-7613(1975)3 2.0.CO;2 Article history first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Frederic L. Schwab; Framework mineralogy and chemical composition of continental margin-type sandstone. Geology 1975;; 3 (9): 487–490. doi: https://doi.org/10.1130/0091-7613(1975)3 2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Compositional data for modern deep-sea sand and ancient graywacke were used by Crook to postulate that Atlantic, Andean, and western Pacific continental margin types could be distinguished on the basis of unique composition—a progressive decrease in framework quartz, total SiO2, and K2O/Na2O ratio. A consideration of the major source areas generated by plate tectonics mechanisms suggests that the premise is valid and can be expanded to include sandstone varieties other than gray-wacke, but more data on modern sand are needed to refine the concept. The potential usefulness of such contrasts in sandstone mineralogy and chemistry is demonstrated by comparing the composition of several ancient sandstone units (mainly from the Appalachian-Caledonian belt) for which plate tectonics basin models have been proposed. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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