FRANKLIN AND STERLING HILL NEW JERSEY: THE WORLD'S MOST MAGNIFICENT MINERAL DEPOSITS
HOME MINERAL INDEX SEARCH LINKS BIBLIOGRAPHY INTRODUCTION CULTURAL ASPECTS LOCAL GEOLOGY GEOLOGY OF THE ZINC DEPOSITS
GEOCHEMISTRY FLUORESCENCE THE MINERAL ASSEMBLAGES LISTS OF MINERALS DESCRIPTIVE MINERALOGY NESOSILICATES
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


The olivine group

FAYALITE

FORSTERITE

TEPHROITE

GLAUCOCHROITE

 

The humite group

NORBERGITE

CHONDRODITE

HUMITE

CLINOHUMITE

 

The manganese-humite and leucophoenicite groups

ALLEGHANYITE

MANGANHUMITE

SONOLITE

LEUCOPHOENICITE

JERRYGIBBSITE

 

The garnet group

ALMANDINE

ANDRADITE

GROSSULAR

GOLDMANITE

SPESSARTINE

 

Other nesosilicates

BAKERITE

BULTFONTEINITE

CHLORITOID

CLINOHEDRITE

DATOLITE

ESPERITE

GENTHELVITE

GERSTMANNITE

HODGKINSONITE

HOLDENITE

KOLICITE

LARSENITE

SILLIMANITE

THORITE

TITANITE

URANOPHANE

WILLEMITE

YEATMANITE

ZIRCON

 

GENTHELVITE

Zn4Be3(SiO4)3S
Cubic   

Genthelvite, a rare zinc beryllium sulfur silicate mineral of the helvite group, was reported from Franklin by Essene and Peacor (1987) as microscopic grains associated with gahnite, sphalerite, titanite, petedunnite, and numerous other minerals. It has not been reported from Sterling Hill. It was observed to be isotropic, with brilliant blue cathodoluminescence in the electron beam. It was identified on the basis of EDS analysis and its isotropic behavior. Genthelvite is apparently a very rare mineral at Franklin and has been found in only one very atypical sample which, though assuredly from Franklin, is not representative of Franklin specimens.

 

FOOTER LBI

 
Copyright © 1995 by Pete J. Dunn
Website by Herb Yeates
 
Link to homepage
This page created: January 11, 2001

 

CHAPTER 15. NESOSILICATES