FRANKLIN AND STERLING HILL NEW JERSEY: THE WORLD'S MOST MAGNIFICENT MINERAL DEPOSITS
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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


SOROSILICATES

The epidote group

ALLANITE-(Ce)

CLINOZOISITE

EPIDOTE

HANCOCKITE

PIEMONTITE


Other sorosilicates

BARYLITE

BARYSILITE

CUSPIDINE

FERROAXINITE

GANOMALITE

HARDYSTONITE

HEMIMORPHITE

JUNITOITE

KENTROLITE

MANGANAXINITE

NASONITE

PUMPELLYITE-(Mg)

SAMFOWLERITE

THORTVEITITE

VESUVIANITE


CYCLOSILICATES

The tourmaline group

DRAVITE

SCHORL

UVITE

 

FERROAXINITE

Ca2FeAl2BSi4O15(OH) 
Triclinic

 
 
 
  Figure 16-6. Crystal drawings of ferroaxinite from the Gooseberry Mine in Franklin. These drawings, projections of the same crystal, are from Palache (1935) who provided crystallographic data.  
   

Ferroaxinite, a calcium iron aluminum boron silicate hydroxide mineral of the axinite group, is rare at Franklin. Palache (1935) reported it as crystals (Figure 16-6) from the Gooseberry Mine, one of a string of magnetite deposits just south of the Franklin Mine; this material has not been restudied.

At the Franklin mine, ferroaxinite is found in the Palmer Shaft area as euhedral, light-brown to medium brown crystals associated with hedenbergite, epidote, end-member zircon, andradite, pyrite, and fluorapophyllite. Partial microprobe analysis of these crystals confirms they are ferroaxinite, with 4 wt. % MnO, 1 wt. % MgO, and no appreciable zinc. 

 

 

 

 

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Copyright © 1995 by Pete J. Dunn
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This page created: January 11, 2001

 

CHAPTER 16. SOROSILICATES AND CYCLOSILICATES