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zn-pb
The thermodynamic simulations were conducted for the system H-O-K-Na-Ca-Mg-Al-Si-Fe-C-Cl-S-Zn-Pb-Cu, which is described by 54 minerals of constant and variable composition and 78 aqueous species.
      
Hydrodynamic and geochemical conditions of the formation of stratiform Zn-Pb ore mineralization by chloride solutions
      
Gas evolution of electrodeposited Zn-Pb-In-Bi alloy powder was less than that of atomized mercury-free alloy powder.
      
The hydrothermal activity which began in this steam explosion center is responsible for the formation of the Kuroko-type Cu-Zn-Pb-mineral deposits.
      
The various Zn-Pb-Ba-Fe occurrences appear to be strictly bound to continental dolomitic sediments (black ferroan dolomites), which outline the triassic erosional surfaces.
      
Comments on the genesis of the Eastern-Alpine Zn-Pb deposits
      
Most of the Cu-Fe skarn deposits studied were formed under pressures of more than 1 kb, whereas Zn-Pb(-Cu-Fe) deposits tend to have formed at relatively shallow environments, namely under less than 1 kb.
      
The massive Fe-Zn-Pb sulphide sheets constituting the Angel Zone ore body of the Black Angel Mine, show evidence of three phases of deformation at greenschist facies metamorphic grade.
      
Le gisement Zn-Pb de Trèves est situé dans le Lias de la bordure orientale des Causses (Sud-Est du Massif Central fran?ais).
      
No exhalative Cu-Zn or Zn-Pb ore has been discovered associated with the submarine volcanic stratabound Cu-rich alteration zone.
      
Ore petrology and metamorphic history of Zn-Pb ores, Monteneve, Tyrol, N.
      
These intrusives are cross-cut by polymetallic ore veins (Fe-Cu-Zn-Pb), and are hydrothermally altered in association with the mineralization.
      
Sulfide - carbonate relationships in the Navan (Tara) Zn-Pb deposit, Ireland
      
Stratiform Zn-Pb-Cu mineralization is underlain by Cu-bearing stockwork ore and an extensive alteration zone.
      
A regional fluid inclusion study of Cu-Au (+Zn-Pb) mineralisation in the Harlech Dome area, North Wales, gives support to the concept of two distinct metallogenic episodes.
      
Sulfur and carbon isotope compositions in the stratiform Zn-Pb-Cu sulfide deposits of the Rajpura-Dariba belt, Rajasthan, NW Ind
      
Macrotextures, microtextures, and carbonate-sulfide relationships in stratiform, carbonate-hosted Zn-Pb orebodies of Silvermines
      
Replacement of dolomite rhombs is zone selective in Cracow-Silesian Zn-Pb deposits.
      
The lead isotope composition of three Cu-Zn-Pb sulfide deposits and one Au deposit in the Early Proterozoic Svecofennian of central Sweden reveals the existence of two distinct lead sources in the region.
      
Peloids in stratabound Zn-Pb deposits and their genetic importance
      
 

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