normal merensky reef in proximity to the regional pothole
TRANSCRIPT
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Normal Merensky Reef in Proximity to the Regional Pothole Sub-Facies of the Zwartklip Facies, Upper
Critical Zone, Western Bushveld Complex
D. S. SmithGeology Department, Northam Platinum Mine
I. J. Basson * and D. L. ReidDepartment of Geological Sciences, University of Cape Town
(* Presenting)
GEOLOGY
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Modified after Viljoen (1994), Eales and Cawthorn (1996), Viring and Cowell (1999)
GEOLOGY
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Modified after Viring and Cowell (1999)GEOLOGY
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GEOLOGY
Planar MCU Bottom Chromitite(“4A/Upper Chromitite”)
(Cryptic lamination in upper 20 cmof Inter-Chromitite pegmatoid)
Heterogeneous, medium-grained/pegmatoidal harzburgite
More homogeneous, medium-grained/pegmatoidal harzburgite
Undulating granular orthocumulate chromitite (“4X/Lower Chromitite”)
Mottled anorthosite
Typical section and PGE g profile through Normal Merensky Reef (note that the Inter-Chromitite harzburgite and dunite are not developed in this example)
140 cm
MCU poikilitic pyroxenite
(coarse, clustered sulphides)
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Compiled from 1:1000 and 1:200 Scale Geological Maps
GEOLOGY
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Compiled from underground observations by Geology and Sampling Departments
GEOLOGY
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Oasis Montaj Plots of data obtained by Geology and Sampling Departments
GEOLOGY
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Oasis Montaj Plots of data obtained by Geology and Sampling Departments
GEOLOGY
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Oasis Montaj Plots of data obtained by Geology and Sampling Departments
GEOLOGY
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Oasis Montaj Plots of data obtained by Geology and Sampling Departments
GEOLOGY
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Data obtained by Geology and Sampling Departments
N=1889GEOLOGY
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Data obtained by Geology and Sampling Departments
N=1889GEOLOGY
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Data obtained by Geology and Sampling Departments
N=1889GEOLOGY
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Data obtained by Geology and Sampling Departments
N=1889GEOLOGY
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GEOLOGY
Conclusions- Systematic changes in reef morphology/lithologies are evident in the 320 cm to 0 cm reef
thickness interval; these include the loss of the medium-grained pegmatoidal orthopyroxenitein the 300-160 cm thickness interval
- Relatively dramatic changes in reef morphology, PGE g and Grade occur belowInter-Chromitite reef thickness of 160 cm, possibly corresponding to the thermomechanical“breaching” of a relatively impermeable dunite layer
- Total Normal Reef PGE g and Grade correlate strongly with PGE g/Grade of the Inter-Chromitite Pegmatoid
- 4X and Inter-Chromitite Pegmatoid PGE g display lognormal relationships to Reef Thickness
- PGE g and Grade display an inverse (lognormal) relationship to one another
- A PGE-rich sulphide zone above the 4X/Lower Chromitite becomes progressively more evidentwith reef thinning and is included in routine sampling of the 4X Chromitite – prioritising theextraction of the lower chromitite, based on such data, is probably erroneous when appliedto thicker Normal Reef
- The 4A/Upper Chromitite (Merensky Chromitite) is a “drape” and has a regular/consistentPGE content and is usually more planar than the undulating 4X chromitite