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lead-zinc deposits
New mineralogical and geochemical data on lead-zinc deposits of the Sadon ore field, north Ossetia
      
Discovery of seismites in Upper Sinian stratiform lead-zinc deposits in Dadu River valley, Sichuan, China: Implication for ore g
      
The Broken Hill Lode, located in western New South Wales, is one of the largest silver-lead-zinc deposits in the world.
      
Diagenetic pyrite from the lead-zinc deposits of Zawar, India
      
Pyrite from the Precambrian lead-zinc deposits of Zawar, West India, shows excellent sedimentary features, viz., composite bedding, lenticular bedding, flame structure etc.
      
Large gas-liquid inclusions are found in the galena crystals from some hydrothermal lead-zinc deposits.
      
Empirical support for the sedimentary formation of pyrrhotite is provided by textural and qualitative mineralogical data from Mount Isa and other stratiform lead-zinc deposits.
      
Lead-zinc deposits are localized within Albian to lower Cenomanian sedimentary sequences of the Cretaceous Benue trough which formed in the middle of the Pan-African Nigerian shield.
      
Lithogeochemical exploration for shale-hosted lead-zinc deposits: Case studies from the McArthur River and Mt Isa Districts, nor
      
The large lead-zinc deposits of Middle Proterozoic age in northern Australia occur in sediments interpreted as having been deposited under saline, shallow-emergent conditions.
      
Pyritic shale horizons of the Newland Formation (Belt Series, Mid-Proterozoic) show striking similarities to Proterozoic pyritic shales elsewhere that are host to major lead-zinc deposits, such as Mt.
      
Basinal brines and groundwaters as possible metal carriers in the formation of sandstone-hosted lead-zinc deposits
      
Pyrite deformation in stratiform lead-zinc deposits of the Canadian Cordillera
      
Application of this technique allows the identification of low-molecular-weight n-alkanes and some aromatic hydrocarbons in sulfides and gangue minerals from epigenetic Variscan and post-Variscan lead-zinc deposits in the Rhenish Massif, Germany.
      
Remarkable advances in age dating Mississippi Valley-type (MVT) lead-zinc deposits provide a new opportunity to understand how and where these deposits form in the Earth's crust.
      
The contrast in abundance between SEDEX and MVT lead-zinc deposits in the Proterozoic questions the frequently suggested notion that the two types of ores share similar genetic paths.
      
A majority of the world's sediment-hosted exhalative (SEDEX) lead-zinc deposits are vent-distal.
      
Discussion on "Mississippi Valley-type lead-zinc deposits through geological time: implications from recent age-dating research"
      
Reply to Discussion on "Mississippi Valley-type lead-zinc deposits through geological time: implications from recent age-dating
      
Whiskers and thin platelets of pyrite have been found growing coherently on the face of small cubic pyrite crystals from the Strashimir and Gradishte hydrothermal lead-zinc deposits.
      
 

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