X-ray spectrochemical analysis: An application to certain light elements in clay minerals and volcanic glass
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Volcanic glass
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Characteristics and conditions of accumulation of clay minerals in Maykopian series of Predkavkaz'ye
The clay minerals of the Maykopian succession, regionally oil bearing, have been studied, with staining, optical, thermal (DTA), microscope, electron microscope, X-ray and electron diffraction methods. The data obtained suggest that the composition and distribution of clay minerals in the Maykopian are connected with two basic factors: First, a definite regularity in the variation in clay minerals in the borehole section exists, depending on their position in a particular geotectonic zone; second, the minerals are characteristic of definite mineral provenances and reflect differences in provenance. J.J. Finney
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Other| June 01, 1978 X-ray identification of clay materials in thin sections M. J. Wilson; M. J. Wilson Search for other works by this author on: GSW Google Scholar D. R. Clark D. R. Clark Search for other works by this author on: GSW Google Scholar Author and Article Information M. J. Wilson D. R. Clark Publisher: SEPM Society for Sedimentary Geology First Online: 03 Mar 2017 Online ISSN: 1938-3681 Print ISSN: 1527-1404 GeoRef, Copyright 2006, American Geological Institute. Journal of Sedimentary Research (1978) 48 (2): 656–660. https://doi.org/10.1306/212F7513-2B24-11D7-8648000102C1865D Article history First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation M. J. Wilson, D. R. Clark; X-ray identification of clay materials in thin sections. Journal of Sedimentary Research 1978;; 48 (2): 656–660. doi: https://doi.org/10.1306/212F7513-2B24-11D7-8648000102C1865D 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 SocietyJournal of Sedimentary Research Search Advanced Search Abstract A method is described which allows X-ray powder diffraction information to be obtained directly from small areas of clay minerals and other fine-grained material in petrographic and soil thin-sections. 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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