5. Pep e 1 A. - Niekt6re' problemy opracowania fal zalamanych . zwU}zanych ze stropem karbonu. Techn. Posz. 1966, nr 18.
6. S k 0 r u p a J. ...l. Modologia sironsolldowanego pocUoza w Polace, w §wietle sejsmiezn.ych prac re-frakcyjnych (referat wygloszony
na
ses!i po§wi~ conej problematyce skorupy i g6rnego plaszcza Ziemi, zorganizowanej przez Z. G. PAN w 1968 r. (w druku) . .SUMMARY
Contrary to. the old cystalline basement of the East-European platform, the consolidation degree of the Eocambrian basement (eastern part of the Car-pathian Foreland) and of the Variscan basement (Fore-Sudetic Monoc1ine, Opole Trough, Upper SUe-si8lll Basin, and North-Sudetic Trough) is much lower. In the case of the old Pre-Cambrian basement
. we find, in the refraction works, a wave that may practically be thought to represent a frontal wave gliding in the top portion, whereas in the case of the Eocambrian (Assintian) and Variscan basements a distimct occurrence of rather deeply reaching refracted waves may be observed. The parameters of these waves depend upon the consolidation degree of the basement. On the basiS of the works so far performed in the southern area of Poland, where some refracted waves for the basement have been
detected, the present author gives their parameters, and compares them with the boundary velocities for
the top of the basement. .
The above data presented graphically demonstrate that here some dependences exist, and that we may precisely draw the "calibration curves", which' cha-racterize the consolidation degree of a given type of the basement. The author suggests that the retracted waves may be used also in the examination of the local consolidation degree of the basement. This has also some practical aspects, e.g. in oU prospections. Moreover, the author discusses the effectiveness of various ways in presenting the results obtaiJned, in relation to the examination of the consolidation degree of the basement.
7. Skorupa J., Wronicz S. - Motliwo§cl me-todyczne i wyniki prac refrakcyjnych w obBzarze monokliny przedsudeckiej i' niecki
p6lnocDosudec-kiej. Arch. IG, 1968. .
8. S k 0 r u p a J. - Pr6ba reinterpretacji profilu regionalnego IG 1 w odniesieniu do stropu skon-solidowanego podloZa. Ibidem.
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