Faults & Folds
As
coal deposits form a fairly brittle ore body, when they are subjected
to major tectonic disturbances such as faulting, folding and shearing,
they can suffer a high degree of fracture with low shear resistance.
To support this, outburst studies show that the presence of fractures
and shear zones coexist with outburst prone areas. The shear zones indicate
the presence of excess stress and planes of weakness and also the existence
of pockets of gas and pulverised coal (Doyle,
2002).
All
fatal outbursts in Australia (except Leichhardt Colliery) have occurred
on faults. This is not to say that all faults will show the occurrence
of outburst. The types of faults most likely to be associated with
outbursts are low angle reverse faults and strike-slip faults. Between
the faults, mining conditions are generally good. The magnitude of
the fault often bears no relationship to the magnitude of the outburst. |