Jk. Schweitzer et Ra. Johnson, GEOTECHNICAL CLASSIFICATION OF DEEP AND ULTRA-DEEP WITWATERSRAND MINING AREAS, SOUTH-AFRICA, Mineralium Deposita, 32(4), 1997, pp. 335-348
As depth of mining increases, so the production costs of the aurifereo
us Witwatersrand deposits are continuously increasing, with some mines
already mining at depths exceeding 3500 m. Health and safety aspects
are, simultaneously, gaining in importance. Therefore, in order to min
e deep orebodies in existing mines, as well as to develop new mining v
entures safely and efficiently, novel approaches, including mining str
ategies, layouts and support systems have to be adopted. Geological fe
atures largely control the deformation mechanisms associated with Witw
atersrand orebodies. These features are grouped into two major categor
ies: primary and secondary features. Both impact on the rockmass behav
iour associated with the excavations, and contribute to the definition
of geotechnical areas. Primary geological features are defined by the
various rock types, orebody geometry, and the frequency and mineralog
ical characteristics of sedimentary structures (e.g. various kinds of
bedding planes and lithological boundaries). The primary features also
control rock engineering properties, closure rates, attitude and freq
uency of mining-induced stress fracturing, and planes may be reactivat
ed during seismic events. Secondary geological features are faults, dy
kes and veins/joints, and associated metamorphism. These cause stabili
ty problems and are often associated with seismic events. Compositiona
l and textural characteristics of these features, and their controls o
n the rockmass behaviour, are ill-defined, Primary and secondary geolo
gical characteristics also play an important role in identifying the a
ppropriate mining strategy, layout and support. Geological features ca
n be predicted into deep unmined areas, and therefore contribute to th
e safest and most efficient extraction of the orebody. Witwatersrand o
rebodies are mined in complex geological environments, with the rockma
ss behaviour differing from one orebody to the other. This is approach
ed by employing a new methodology that attempts to quantify the proble
ms encountered when mining the major Witwatersrand orebodies.