75
4 Characteristics and Formation Process
In addition to cobalt, manganese crusts are a potential source of many other metal elements such as titanium, nickel, rare earths (in particular cerium), zirconium,
molybdenum, vanadium, tellurium, thallium and phosphorus.
Over and above the academic interest of these data, it is justifiable to attempt to
determine the economic potential. Estimations show that a potentially economic
site should have cobalt concentrations of over 1 % and platinum concentrations of
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Fig. 4.5 Diagram illustrating the genesis of hydrogenetic crusts through the formation of complexes and colloidal phases facilitating the absorption of metals
4 Characteristics and Formation Process
In addition to cobalt, manganese crusts are a potential source of many other metal elements such as titanium, nickel, rare earths (in particular cerium), zirconium,
molybdenum, vanadium, tellurium, thallium and phosphorus.
Over and above the academic interest of these data, it is justifiable to attempt to
determine the economic potential. Estimations show that a potentially economic
site should have cobalt concentrations of over 1 % and platinum concentrations of
=RQHGHPLQLPXP
G¶R[\JqQHHW
HQULFKLHHQ0Q
2[\GDWLRQGH0Q
HWIRUPDWLRQGHFROORwGHV
3UpFLSLDWLRQVG¶R[\GHV
HWG¶R[\K\GUR[LGHV
6XEVWUDWGXU
EDVDOWLTXHRXFDOFDLUH
&URWHIHUUR
PDQJQpVLIqUHG¶RULJLQH
K\GURJpQpWLTXH
Fig. 4.5 Diagram illustrating the genesis of hydrogenetic crusts through the formation of complexes and colloidal phases facilitating the absorption of metals
