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

 

GANOMALITE

Pb9Ca5MnSi9O33 
Hexagonal, P3, a = 9.82, c = 10.13 Å, Z = 1.

 
 
 
  Figure 16-7. Tabular, hexagonal ganomalite crystals from Franklin. Field of view is 1.0 mm in maximum dimension.  
   

Ganomalite was first reported from Franklin by Dunn (1979b), and the species was subsequently redefined by Dunn et al. (1985a); it had previously been considered an analogue of nasonite, in error. It was further discussed, within the context of the other lead silicates from Franklin, by Dunn (1985b).

Crystal structure

Preliminary details of the crystal structure of Franklin ganomalite were given by Dunn et al. (1985a). There are four large-cation sites with octahedral coordination, and Mn is ordered in a site of rank 1.

Description

 
 
 
  Figure 16-8. Platy barysilite crystals epitactic on tabular ganomalite crystals from Franklin. Field of view is approximately 0.3 mm in maximum dimension.  
   

Ganomalite occurs as simple hexagonal, tabular, 0.5 mm crystals, mostly in arrays in subparallel growth (Figures 16-7 and 16-8); additional morphological observations and illustrations were given by Yeates (1991).

It is colorless with adamantine luster; cleavage is indiscernible. There is no discernible fluorescence in ultraviolet. Local ganomalite is tentatively distinguished from nasonite by its tabular habit.

Composition

Ganomalite is a lead manganese calcium silicate mineral. Manganese was shown to be an essential constituent of ganomalite by Dunn et al. (1985a). There is little or no solid solution of other cations. An analysis is presented in Table 8.

Occurrence and paragenesis

At Franklin, ganomalite occurs in andradite, associated with nasonite and clinohedrite; few specimens are known. Ganomalite crystals occur freely-formed within vugs (Figure 16-7) and also enclosed within massive clinohedrite, the study of which revealed the coexistence of euhedral nasonite and ganomalite in contact. Aside from the above assemblage, ganomalite was seen in one anomalous specimen of the larsenite assemblage, associated with late-stage barysilite and larsenite in a vug.

 

FOOTER LBI

 
Copyright © 1995 by Pete J. Dunn
Website by Herb Yeates
 
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This page created: January 12, 2001

 

CHAPTER 16. SOROSILICATES AND CYCLOSILICATES