Geology
Geology plays a very important role in the manifestation
of Outbursts. Seams having complex geological structures are more prone
to outbursts if high gas conditions are prevalent. The following points
need attention when geological factors are being considered.
• Any structure related to horizontal movement of beds within the coal
seams, presence of soft coal beds in the seam(s) and the thickness.
• Presence of thrust faulting, thickness of the gauge and width of the
fracture zone. Thrust faults of<0.1m thickness are reported not outburst prone
in some mines, but this is not a definite conclusion as the thickness of the
gouge can vary suddenly at the same place through the seam thickness from roof
to floor(Lama, 1980).
• Outbursts have occurred in seams of varying thickness including seams
as thin as 0.5m. Outbursts are more frequent where the seam starts thinning out
or maximum thickness is reached.
• Normal faults which have a throw greater than the seam thickness result
in complete stoppage of gas flow (gas trap) and are more dangerous, than those
with throw less than the seam thickness. Clear faults without any gouge are less
dangerous and greater the thickness of the gauge the greater are the chances
of outbursts. Strike slip faults generate more gouge than thrust faults and gauge
thickness is lower on the normal faults.
•The presence of cleat in coal, particularly shearing of the cleat and
presence of fine sheared material between the cleat surfaces (Wood and Hanes,
1982) is an indication of high stresses and deformation to which the seam is
subjected.
• Seams which are surrounded by sandstone layers have a higher probability
of shearing. Shale and softer rocks tend to protect the seam from shearing and
hence reduce the chances of an Outburst.
• Micro-porosity of coal seams also affects the Outburst pronenss of the
seam. Micro-porosity determines the capacity of the coal to sorb gas as well
as its permeability at matrix level. Coal containing mean pore size radius <75µm
are thought to be more liable to Outburst. Coal seams liable to Outburst have
higher percentages of Clarain. These have highly fractured coal plys(layers)
with high density of micro-cracking (>7mm/mm²). Seams not liable
to Outbursts have crack density <3mm/mm². Seams where the structure has
been damaged or completely obliterated are most liable to Outbursts. (Lama & Bodziony,
1996)
• Determination of the presence of structures such as faults, dykes and
sills is a common practice in general geological investigation prior to the opening
of the deposit. Sheared zones due to folding and faulting usually have upto three
metres of cintred coal (a brownish and weak formation known as Mylonite). This
needs to be investigated carefully
• Seams with Prodyakonov strength index of f<0.5 are highly liable to
Outburst.(Lama & Bodziony, 1996)
• When a coal bearing area is split into two areas with a major fault,
it is essential that both these areas be examined separately. It is quite possible
that the area on the dip side may have quite different conditions related to
gas regime. |