On the basis of mining-geometrical and morphological analysis it was esteblished that the shape of fracture disturbances may vary due to the development of flexure overbending at the areas adjoining the faults.
How to cite:
Nikulin M.V., Grigorev V.E., Panfilov A.L. Mining and geometric peculiarities of D-E, E2, 5-E3 (E3) disturbances of the Komsomolskaya mine field at the OAO Vorkutaugol // Journal of Mining Institute. 2001. Vol. 146. p. 111-118.
