FRANKLIN AND STERLING HILL NEW JERSEY: THE WORLD'S MOST MAGNIFICENT MINERAL DEPOSITS
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SOROSILICATES AND CYCLOSILICATES INOSILICATES PHYLLOSILICATES TECTOSILICATES AND SILICATES OF UNKNOWN STRUCTURE
ELEMENTS SULFIDES ARSENIDES ANTIMONIDES AND SULFOSALTS OXIDES AND HYDROXIDES HALIDES AND CARBONATES
SULFATES BORATES TUNGSTATES AND MOLYBDATES ARSENATRES ARSENIDES PHOSPHATES AND VANADATES UNNAMED MINERALS


QUARTZ

 

The feldspar group

ALBITE

ANORTHITE

ANORTHOCLASE

CELSIAN

HYALOPHANE

MICROCLINE

OLIGOCLASE

ORTHOCLASE

 

The scapolite group

MARIALITE

MEIONITE

 

The zeolite group

ANALCIME

CHABAZITE

HEULANDITE

LAUMONTITE

NATROLITE

STILBITE

THOMSONITE

 

Silicates with unknown structures

BOSTWICKITE

NEOTOCITE

WAWAYANDAITE

ANALCIME

NaAlSi2O6.H2O
Cubic

Analcime, a sodium aluminum silicate hydrate mineral of the zeolite group, was reported by Frondel (1972) to occur in the camptonite dikes in the Buckwheat Open Cut at Franklin.

 

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Copyright © 1995 by Pete J. Dunn
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CHAPTER 19. TECTOSILICATES AND SILICATES WITH UNKNOWN STRUCTURE