RESEARCH GROUP

button mineral resources
Mineral Resources and Geofluids
 

Ore Deposits Introductory Course

Prof. Lluís Fontboté and collaborators

 

Slides to Chapter Q

Supergene alteration and enrichment processes

 

Rodalquilar

Goethite crusts in fracture joints in the open pit 2 of the old Transaction Mine, Rodalquilar, Almería, Spain.
François Martin, 2007.05/63
Click on the picture for an enlarged version of this photograph

Rodalquilar

Colorful iridescences of Fe-hydroxides (possibly goethite or lepidocrocite) formed on a rock surface.
Note that the colors are caused by interference of the very thin layers of the Fe-hydroxides with light
and not by trace element contents. Open pit 2, Transaction mine, Rodalquilar District, Spain.
Copyright © 2000 - Laurie Cortesi - All Rights Reserved.

Rodalquilar

Colorful iridescences of Fe-hydroxides (possibly goethite or lepidocrocite) formed on a rock surface.
Note that the colors are caused by interference of the very thin layers of the Fe-hydroxides with light
and not by trace element contents. Open pit 2, Transaction mine, Rodalquilar District, Spain.
Copyright © 2000 - Laurie Cortesi - All Rights Reserved.

Rodalquilar

Colorful iridescences of Fe-hydroxides (possibly goethite or lepidocrocite) formed on a rock surface.
Note that the colors are caused by interference of the very thin layers of the Fe-hydroxides with light
and not by trace element contents. Open pit 2, Transaction mine, Rodalquilar District, Spain.
Copyright © François Martin, 2007.05/63 - All Rights Reserved.
Click for a large image

Lobo

Liesegang rings following fractures on an altered volcanic rock at the Lobo Au-deposit, Maricunga Belt, northern Chile.
Photo Lluís Fontboté, 1994.10-3/06 Copyright © 1999 - Lluís Fontboté - All Rights Reserved.

 

[Mineral Resources and Geofluids]

 


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