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


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

DJURLEITE

Cu31S16
Monoclinic

Djurleite, a copper sulfide mineral, was first reported from Franklin by Cook (1973). It was found associated with dolomite and hematite in a vein in franklinite-willemite  ore. No other data were given. Djurleite was reported from Sterling Hill by Jenkins and Misiur (1994).

The writer has found djurleite on specimens labeled chalcocite; these two grayish-black, opaque, sectile minerals are visually identical and require X-ray techniques for identification. Like chalcocite, djurleite may have a sooty surface coating. Djurleite is far less abundant locally than chalcocite.

 

FOOTER LBI

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

 

CHAPTER 21. SULFIDES, ARSENIDES, ANTIMONIDES, AND SULFOSALTS