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)
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 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 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 mine (Var, France). Typical host rock: Sandstone
beds.
Photo Pierre Perroud, Oct. 1992, n2.
Copyright © 2000 - Pierre Perroud
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
Evaporite pseudomorph. Navan, Ireland, 1984.
© Photo Lluís Fontboté
Click on the picture for an enlarged version of this photograph