Mineralogy and Geology of Natural Zeolites / / ed. by Fred A. Mumpton.

• Superior document: Title is part of eBook package: De Gruyter DGBA Physical Sciences <1990
• MitwirkendeR: Boles, James R.,; Flanigen, E. M.,; Flanigen, Edith M.,; Hay, R. L.,; Mumpton, F. A.,; Sheppard, R. A.,; Surdam, Ronald C.,
• HerausgeberIn: Mumpton, Fred A.,
• Place / Publishing House: Berlin ;, Boston : : De Gruyter, , [2018]; ©1977
• Year of Publication: 2018
• Language: English
• Series: Reviews in Mineralogy & Geochemistry , 4
• Physical Description: 1 online resource (XII, 233 p.)
• Other title: Frontmatter --; Preface and Acknowledgments --; Copyright --; Additional Copies --; Table of Contents --; Recommended References --; Chapter 1. NATURAL ZEOLITES --; Chapter 2. CRYSTAL STRUCTURE AND CHEMISTRY OF NATURAL ZEOLITES --; Chapter 3. GEOLOGY OF ZEOLITES IN SEDIMENTARY ROCKS --; Chapter 4. ZEOLITES IN CLOSED HYDROLOGIC SYSTEMS --; Chapter 5. ZEOLITES IN OPEN HYDR0L0GIC SYSTEMS --; Chapter 6. ZEOLITES IN LOW-GRADE METAMORPHIC GRADES --; Chapter 7. ZEOLITES IN DEEP-SEA SEDIMENTS --; Chapter 8. COMMERCIAL PROPERTIES OF NATURAL ZEOLITES --; Chapter 9. UTILIZATION OF NATURAL ZEOLITES --; Appendix I. REPRESENTATIONS AND MODELS OF ZEOLITE CRYSTAL STRUCTURES --; Appendix II. CRYSTAL STRUCTURE DATA FOR IMPORTANT ZEOLITES --; Tables: 1-22
• Format: Mode of access: Internet via World Wide Web.
• ISBN: 9781501508585; 9783110637243
• ISSN: 1529-6466
• DOI: 10.1515/9781501508585
• Access: restricted access
• Hierarchical level: Monograph
• Statement of Responsibility: ed. by Fred A. Mumpton.

Volume 4 of Reviews in Mineralogy was prepared to serve as notes for a short course on the Mineralogy and Geology of Natural Zeolites held in Seattle, Washington, November 4-6, 1977. The title of the short course reads Natural Zeolites; however, the subject matter treated in the course and reviewed here deals primarily with those zeolites that occur in sedimentary rocks and which have formed by authigenic or burial diagenetic processes. Unfortunately, only limited coverage has been given to the classical occurrences of zeolites--the megascopic crystals in the vugs and cavities of basalts and other basic igneous rocks. Our only justification is that since the late 1950s, almost all major efforts on zeolites have been directed towards the "sedimentary" occurrences, and it is these occurrences of zeolites in sedimentary rocks that are still unfamiliar to many geologists and mineralogists. It is our intention that this short course and these notes will play a small role in alleviating this unfamiliarity.