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Diamond Deposit Model
e.g. Kimberley Mine (South Africa), Argyle Mine (Australia)


Adapted from Evans 1997: Ore Geology and Industrial Minerals


A study of diamond deposit's tectonic setting shows that diamond bearing kimberlites are restricted to Archean cratons while diamond bearing lamproites are restricted to Proterozoic mobile belts adjacent to cratons.
Kimberlites are much more important in terms of their number and subsequent production of diamonds however those lamproites which have been found proved to be very productive, for example the successful Argyle mine which is a lamproite based.

Kimberlite is a potassic, ultrabasic, hybrid igneous rock containing amongst others, megacrysts of olivine, enstatite and phlogopite in a fine grained matrix of olivine, phlogopite, calcite, serpentinite, spinel and ilmenite.
Lamproite is a potassium and magnesium rich lamprophyric rock containing clinopyroxene, amphibole, phlogopite, olivine and sanidine either as megacrysts or groundmass.



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