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


The halides

ATACAMITE

FLUORITE


The carbonates


The calcite group

CALCITE

OTAVITE

RHODOCHROSITE

SIDERITE

SMITHSONITE


The dolomite group

DOLOMITE

KUTNAHORITE


Other carbonates

ARAGONITE

AURICHALCITE

AZURITE

CANAVESITE

CERUSSITE 

DYPINGITE

HYDROTALCITE

HYDROZINCITE

LOSEYITE

MALACHITE

MONOHYDROCALCITE

PYROAURITE

ROSASITE

SCLARITE

SJÖGRENITE

STRONTIANITE

ZNUCALITE

SJÖGRENITE

Mg6Fe3+2(CO3)(OH)16.4H2
Hexagonal

 
 
 
  Figure 23-27. Platy, sharp-edged crystals of sjögrenite, overgrown on ragged-edged crystals of pyroaurite from Sterling Hill. Field of view is 0.6 mm in maximum dimension.  
   

Sjögrenite, a magnesium ferric-iron carbonate hydroxide hydrate mineral and a polymorph of pyroaurite, was first noted from Sterling Hill by Dunn and Leavens (1981); it has not been found at Franklin. The crystals are bright orange, with vitreous luster, and occur as sharp-edged, stacked, platy crystals overgrown epitactically on corroded pyroaurite (Figure 23-27).

Sjögrenite was verified using powder X-ray diffraction methods and chemical tests. It is best distinguished from pyroaurite using X-ray methods.

The above-described sjögrenite occurs on the 1300 level at Sterling Hill, on a matrix of calcite- willemite-franklinite  ore, which is coated with secondary chlorophoenicite, sphalerite, barite, willemite, and pyroaurite. Sjögrenite is a rare mineral locally.

 

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

 

CHAPTER 23. HALIDES AND CARBONATES