Gottardiite, a new high-silica zeolite from Antarctica: the natural counterpart of synthetic NU-87
Gottardiite was discovered in the Jurassic Ferrar dolerites of Mt. Adamson (Northern Victoria Land, Antarctica). The new zeolite occurs as subparallel aggregates of transparent pseudo-hexagonal lamellae. The mineral is orthorhombic, space group Cmca, with a=13.698(2), b=25.213(3), and c=22.660(2) Å...
Main Authors: | , , , |
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Other Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1996
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Subjects: | |
Online Access: | http://hdl.handle.net/11380/736688 |