Distribution and Origin of the "Gypsum Line" in the Valley Copper Porphyry Deposit, Highland Valley, British Columbia

1976 ◽  
Author(s):  
J L Jambor ◽  
W J McMillan
2018 ◽  
Vol 56 ◽  
pp. 04017
Author(s):  
Natalya Lavrik ◽  
Natalya Litvinova ◽  
Tatyana Aleksandrova ◽  
Valentina Stepanova ◽  
Alexandra Lavrik

In this article shown platinum mineralization comparative characteristics for three deposits: Kondoer-traditional unique deposit and other two probably alternative source of platinum: the Poperechnoe ironmanganese deposit and the Malmyzh copper-porphyry deposit. Platinoids of the Kondoer deposit are the chain Pt>>Ir>Os>Ru=Rh>Pd. The presences of platinum crystals are characteristic, there are over 50 rare and new platinoids minerals in different combinations. There are gold and silver. Platinoids from the iron-manganese ore of Poperechnoe are as Pt>>Rh≈Ir>Ru≈Os>Pd. A scattered dissemination of arsenide sulfate and sulfides of Rh, Ir, Ru, Os are noted in the platinum. Palladium is present as impurities in gold and platinum. The gold content is different-with admixtures Ag, Pb, Cd, Fe. At this stage the platinoids content in oxidized ores of the Malmyzh gold-copper porphyry deposit is Pt ≈ Pd. The gold is present as electrum. There is native silver cadmium.


2019 ◽  
Vol 5 ◽  
pp. 37-48
Author(s):  
I.A. Blinov

Samples of oxidation zone of the Elenovskoe Cu porphyry deposit are studied using optical and scanning electronic microscopy. In addition to Fe hydroxides and abundant malachite, the supergene mineral assemblage includes native Cu and Au, Ag-containing covellite, cuprite, tenorite, plumbogummite, goyazite, iodargyrite, atacamite, and chrysocolla. The oxidized ores contains pyrite relics and high amount of tourmaline (dravite). Some dravite grains contain Cu.


2014 ◽  
Vol 109 (4) ◽  
pp. 859-890 ◽  
Author(s):  
H. E. Pass ◽  
D. R. Cooke ◽  
G. Davidson ◽  
R. Maas ◽  
G. Dipple ◽  
...  

1973 ◽  
Vol 15 (6) ◽  
pp. 660-663 ◽  
Author(s):  
Ye.Z. Meshchaninov ◽  
V.N. Azin

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