Zeolites - Zeolites in Sedimentary Rocks

The American Institute of Mining, Metallurgical, and Petroleum Engineers
Richard A. Sheppard
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: Richard A. Sheppard  (1975)  Zeolites - Zeolites in Sedimentary Rocks

MLA: Richard A. Sheppard Zeolites - Zeolites in Sedimentary Rocks. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1975.

Export
Purchase this Article for $25.00

Create a Guest account to purchase this file
- or -
Log in to your existing Guest account