Abstract
Research Article| January 01, 1896 Solution of Silica Under Atmospheric Conditions* C. Willard Hayes C. Willard Hayes Search for other works by this author on: GSW Google Scholar GSA Bulletin (1896) 8 (1): 213–220. https://doi.org/10.1130/GSAB-8-213 Article history first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation C. Willard Hayes; Solution of Silica Under Atmospheric Conditions. GSA Bulletin 1896;; 8 (1): 213–220. doi: https://doi.org/10.1130/GSAB-8-213 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 SocietyGSA Bulletin Search Advanced Search Abstract Solubility of Silica under other than atmospheric Conditions.It is well known that under conditions prevailing at considerable distances below the earth’s surface silica is one of the more easily soluble of the substances entering into the composition of the earth’s crust. This is shown by the formation of secondary quartz veins, the solution and redeposition of quartz in both sedimentary and crystalline rocks, and, on a large scale, in the replacement of silica by other minerals, as in the case of the iron ores of the Lake Superior region. It is also well known that during the process of rockweathering under atmospheric conditions, by the breaking down of various silicates, much silica passes into solution. Merrill† has shown that in the passage of various crystalline rocks, as diabase and granite, from the fresh condition to that of soil, they suffer a larger absolute loss of silica than of any . . . 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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