10. Pr e i diM. - Budowa tektoniczna obszaru Lu-bina i Sieroszowic. Prz. geoL, 1967, nr 6.
11. S a I ski W. - Metodyka badan mezoskopowych zjawisk tektonicznych w wyrobiskach g6rni-czych. Kwart. geol. (w druku).
12. Tom a s z e w ski J. Tektonika brzeinej SUMMARY
The paper shows a necessity of performing detailed tectonic surveys In mines. The surveys are especially necessary in the case of deposits occurring at
great
depth and characterized by highly complex tectonic structure, which preclude adequate recognition on the basis of borehole data. These factors may be responsible for differences between geological inter-pretation and actual geological setting of a deposit. In such situation the recognition of regularities in the tectonic structure is only possible on the basis of geological data concerning fracturing and fissures faults, folds, and slikensides, gathered in the cours~ of mining works. Current analysis of these data can make possible a more accurate reconstruction of spa-tial distribution of deposits and, hence, to verify the scheme of mine building ~nd exploitation. . .
Knowledge of the tectonic structure is also imor-tant for the solution of some engineering-geological and hydrogeological problems in mining. This is evi-denced by numerous examples from copper mines in the Fore-Sudetic monocline. Moreover, tectonic de-formations have a negatwe effect on the magnitude of loss ofe deposit and they result in impoverishment of ores, particularly when the mining works are highly automatized. Structural stUdies in mines also contribute to both the improvement of methodology of mining works and the recognition of geological structure of a tectonic unit.
cz~ci monokliny przedsudeckiej. Rudy i Met. nieteL, 1963, nr 6.
13. W i e r z c how s k a Z., Z n a
n
ski J. - Pocho-dzenie wstrzl4s6w g6rotworu w Polskim Zaglc:biu· Wc:glowym. Problemy geodynamiki i t/ilPafl. Ko-mitet G6rnictwa PAN, 1972, Krak6w.PE3lOME
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