Zeolites - Zeolites in Sedimentary Rocks

- Organization:
- The American Institute of Mining, Metallurgical, and Petroleum Engineers
- Pages:
- 6
- File Size:
- 351 KB
- Publication Date:
- Jan 1, 1975
Abstract
Zeolites-crystalline hydrated aluminosilicates of the alkalis and alkaline earths-are important rock-forming constituents in sedimentary rocks and are potentially valuable industrial minerals. They have a framework structure that encloses interconnected cavities occupied by the relatively large cations and water molecules. The cations, chiefly sodium, potassium, and calcium, and the water have considerable freedom of movement within the structure and give the zeolite their cation- exchange and reversible-dehydration properties. Some zeolites have essential contents of barium, strontium, or magnesium. The basic structure
Citation
APA:
(1975) Zeolites - Zeolites in Sedimentary RocksMLA: Zeolites - Zeolites in Sedimentary Rocks. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1975.