Kroondal, Marikana - Bushveld Complex

North West Province, South Africa

Main commodities: PGE PGM Cr
New International
Study Tour
  Click on image for details.
Andean Porphyries
Click Here

Click Here

Big discount all books !!!
Available as
No single hard copy book more than  AUD $44.00 (incl. GST)
e-BOOKS also discounted

The Kroondal and Marikana platinum mines are located on the south-western and southern limb of the western lobe of the Bushveld Complex, ~120km NW of Johannesburg, and to the immediate NE and east of the town of Rustenburg in the Northwest Province of South Africa.
(#Location: Kroondal - 25° 42' 20"S, 27° 19' 34"E; Marikana - 25° 44' 17"S, 27° 25' 12"E).

The Kroondal mines exploit the UG2 Reef contained in the Kroondal and Townlands blocks. The Townlands blocks is situated immediately to the NE of Rustenburg, and exploits a 7 km, NW-SE trending strike length of the reef. The Kroondal block is separated from the Townlands block by the 8 km long Bathopele Mine of the separate Rustenburg Section mine complex. Within the Kroondal block, an ~8 km strike length of the UG2 reef is represented, striking WNW-ESE. The Marikana block adjoins the Kroondal block to the east, and covers a strike length of ~6 km. The Kroondal block is in turn, bounded to the east by the separate Western Platinum Marikana mine.

The UG2 Reef outcrops on the Kroondal property and dips to the north at ~9°, and on the Townlands block covers a down dip extent of ~1.5 km, normal to the strike of the reef, before it passes into the Rustenburg Section Thembelani mine at depth. Similarly the Kroondal and Marikana blocks cover a variable width normal to strike of ~2 to 3 km before the reef passes downdip into the Rustenburg Section Siphumele mine area at depth.

The Marikana open pit orebody (exhausted in 2011), measured ~1.5 x 3 km, where the UG2 reef had a basin-like structureon its up-dip eroded margin, dipping toward the centre from all sides at between 10 and 20° to a maximum depth of ~200 m. On the northern margin of this basin-like structure the reef reversed dip and resumed the more usual dip to the north at ~9°

The UG2 reef in all three blocks comprises two mineralised seams, the Main and Leader seams, separated by a one-metre barren pyroxenite zone commonly known as the parting. The overlying Merensky reef is not mined at these operations, as it has largely been eroded.

For background on the geology and mineralisation of the Bushveld Complex, see the separate Bushveld Complex record.

See also the Rustenburg Section and Impala Platinum records for a description of the UG2 reef in the adjoining mines.

The JORC compliant ore reserves and mineral resources at the Kroondal Mine at 30 June, 2012 (Aquarius Platinum 2012) were:
        Proved + probable Reserve - 25.51 Mt @ 2.89 g/t 4E, plus
        Measured + indicated + inferred resource - 16.15 Mt @ 5.94 g/t 4E.

The JORC compliant ore reserves and mineral resources at the Marikana Mine at 30 June, 2012 (Aquarius Platinum 2012) were:
        Proved + probable Reserve - 15.61 Mt @ 3.14 g/t 4E, plus
        Measured + indicated + inferred resource - 16.53 Mt @ 5.04 g/t 4E,

Note: 4E = Pt+Pd+Rh+Au,

The most recent source geological information used to prepare this summary was dated: 2012.    
This description is a summary from published sources, the chief of which are listed below.
© Copyright Porter GeoConsultancy Pty Ltd.   Unauthorised copying, reproduction, storage or dissemination prohibited.

  References & Additional Information

Top | Search Again | PGC Home | Terms & Conditions

PGC Logo
Porter GeoConsultancy Pty Ltd
 International Study Tours
     Tour photo albums
 Ore deposit database
 Conferences & publications
PGC Publishing
 Our books  &  bookshop
     Iron oxide copper-gold series
     Super-porphyry series
     Porhyry & Hydrothermal Cu-Au
 Ore deposit literature
 What's new
 Site map