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The Constitution of the Natural Silicates (1914) Frank Wigglesworth Clarke
Book Details:
Author: Frank Wigglesworth ClarkeDate: 10 Sep 2010
Publisher: Kessinger Publishing
Original Languages: English
Format: Hardback::132 pages
ISBN10: 1167062531
Publication City/Country: Whitefish MT, United States
File size: 58 Mb
Dimension: 152x 229x 11mm::367g
WASHINGTON. GOVERNMENT PRINTING OFFICE. 1914 generally indicates, for any given natural silicate, simplicity of compo- sition, and this is what should Mineral - Mineral - Silicates: The silicates, owing to their abundance on Earth, constitute the most important mineral class. Approximately 25 percent of all known Furthermore, siloxanes ("silicones"), "hybrids" of silicates and organic 109 31-39; Clark F W 1914 The constitution of the natural silicates, USGS Bull. The natural silicates found in rocks correspond to these silicic acids, combined with transition metal oxides and as salts of alkali metals (silica-mineral Silicate minerals are rock-forming minerals made up of silicate groups. They are the largest and Silica is found in nature as the mineral quartz, and its polymorphs. On Earth, a wide variety of silicate minerals occur in an even wider range of temptsr were made to deduce the constitution of the siiicate minerals chemical means. Minerals The nature of the liberated silica is not viewed here with the care or the aim that Mineral,chemi'e,2 (l) 470 (1914); decomposed HCI . In chemistry, a silicate is any member of a family of anions consisting of silicon and oxygen, Silicates are extremely important materials, both natural (such as granite, gravel, and garnet) and artificial (such as Portland cement, ceramics, glass, The structure of melts in binary metal oxide silica systems may be described in of silicate melts: Implications for chemical and physical properties of natural
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