FRANKLIN AND STERLING HILL NEW JERSEY: THE WORLD'S MOST MAGNIFICENT MINERAL DEPOSITS
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ELEMENTS SULFIDES ARSENIDES ANTIMONIDES AND SULFOSALTS OXIDES AND HYDROXIDES HALIDES AND CARBONATES
SULFATES BORATES TUNGSTATES AND MOLYBDATES ARSENATRES ARSENIDES PHOSPHATES AND VANADATES UNNAMED MINERALS


Sulfides

ACANTHITE

ARSENOPYRITE

BORNITE

CARROLLITE

CHALCOCITE

CHALCOPYRITE

COVELLITE

DIGENITE

DJURLEITE

GALENA

GERSDORFFITE

GREENOCKITE

HAWLEYITE

MARCASITE

MOLYBDENITE-2H

PYRITE

PYRRHOTITE

SPHALERITE

STIBNITE

WURTZITE


Arsenides and antimonides

BREITHAUPTITE

CUPROSTIBITE

DOMEYKITE

LOELLINGITE

NICKELINE

PARARAMMELSBERGITE

RAMMELSBERGITE

REALGAR

SAFFLORITE

SKUTTERUDITE


Sulfosalts

BAUMHAUERITE

BERTHIERITE

SELIGMANNITE

TENNANTITE

TETRAHEDRITE

ZINKENITE

BAUMHAUERITE

Pb3As4S9 
Triclinic, P1, a = 22.86, b = 8.39, c = 7.94 Ć,
a
= 90, b = 97, g = 90o, Z = 4

 
 
 
  Figure 21-37. Prismatic crystals of baumhauerite from Sterling Hill, growing randomly on platy molybdenite. Field of view is 0.3 mm in maximum dimension. See figure 21-11.  
   

Baumhauerite is a rare mineral from Sterling Hill and is unknown from Franklin.

Description

Baumhauerite occurs as prismatic, acicular, black crystals approximately l mm in length (Figure 21-37). Physical and optical properties were not determined due to the small crystal size and twinning on (100) by reflection. The crystals have a supercell with c = 23.8 Ć (Dr. Joel Grice, pers. comm.).

Composition

Baumhauerite is a lead arsenic sulfide mineral. Sterling Hill material is antimonian with a composition of Pb 50.3, Sb 10.5, As 16.2, S 23.1, total = 100.1 wt. %.

Occurrence and paragenesis

Baumhauerite was found on the 900 level at Sterling Hill by John Kolic. Dissolution of the calcite matrix revealed a number of associated minerals including molybdenite-2H (Figure 21-11), tennantite, arsenopyrite, and seligmannite. Associated gangue minerals are realgar, diopside, barite, fluorapatite and tourmaline. Baumhauerite is commonly associated with molybdenite.

 

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Copyright © 1995 by Pete J. Dunn
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CHAPTER 21. SULFIDES, ARSENIDES, ANTIMONIDES, AND SULFOSALTS