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Mineral Resources and Geofluids
 

Ore Deposits Introductory Course

Prof. Lluís Fontboté and collaborators

 

Slides to Chapter L

Sediment-hosted ore deposits. Part III: Ore deposits formed by basinal brines in clastic and carbonate rocks

Exemple : Mississippi Valley-ore deposits (MVT)

Olkuz

Crustiform ore from the Mississippi Valley-type deposit of Olkusz, Upper Silesia, Poland.
Sphalerite (dark brown and yellow) is the dominant constituent and largely under the colloform variety called Schalenblende.
The sample also contains wurtzite, marcasite, pyrite and galena.
Photo and coll. Pierre Perroud. Copyright © 1999 - Pierre Perroud.

 

Sandstone-hosted Pb-Zn MVT deposit
Cap Garonne Copper mine (Var, France)

Cap Garonne

Cap Garonne mine (Var, France).
North entrance with wiew of the main host rock Triassic fine grained sandstone and pelite.
Photo Pierre Perroud, Oct. 1992, n1. Copyright © 2000 - Pierre Perroud

 

Cap Garonne

Cap Garonne mine (Var, France).
Pillar with alternation of fine grained sandstone and conglomeratic sandstone bearing ore.
Grey: sulfides (tennantite, chalcocite, covellite; galena). Green: Cu sulfates (brochantite, etc.).
Photo Pierre Perroud, Oct. 1992, n3. Copyright © 2000 - Pierre Perroud

Cap Garonne

Cap Garonne mine (Var, France). Typical host rock: Sandstone beds.
Photo Pierre Perroud, Oct. 1992, n2. Copyright © 2000 - Pierre Perroud

 

Cap Garonne

Cap Garonne mine (Var, France). Old tip truck covered with calcium carbide from acetylene lamps.
Photo Pierre Perroud, Oct. 1992, n4. Copyright © 2000 - Pierre Perroud

 

 

Navan

Evaporite pseudomorph. Navan, Ireland, 1984.
© Photo Lluís Fontboté
Click on the picture for an enlarged version of this photograph

 

 

 

[Mineral Resources and Geofluids]

 


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