4. M U
sz
1n
J. A., Cha
t j 8: now F. A., SZlIlerson M. B. Mietodolka pd1s'kow plat-fmmiennych rif~~h massiwow. w .s!oZnyeh siejs-mogieologIC\Zes'lpch uslowijach; Razwledocz-naja Gleoiiz;r.ka,197O, nr~41. I·S. MJlll er P., ~.>W j en h 01 z R. . - 0 gieniezisie uglewodorow w karbonatnych ot~oZenija:ch cech-tlZtiejna: (wiercooiaja !p'ierm) na te:rr'irtorii Gier-'manskoj Demokra'ticzesk~j ReBPUibliki. Gieologija
iNfefti i Gaza, 1968, nr 5.
6; 0 III u C how i C z Z. - Odkrycie zloza ropy na moo.old'infe przedsudec'kiej i dalsze perspektywy poszukiw4n. Prz. geol., 1962, nr 1.
SUMMARY.:
The lIlatu.re of 'lbe record of seIBmic time profileS obtained in the boundary z~ne between rthe
MargmaJ
Syndilnorium and East-Eu'1'opea,n Plalflform is a·na-lysed·. Tbe ana'lyshJ m*es it pda&M.e to diB~h places of ICham:ge in selJsmjc :record. Generally, i!n these pl!QoCf!l9 the dmaoge of ~eated seil9lIlic
'l'e-flec'bor& beccAmes leiE dieat' or; OC'casioolaJily completely dbscure.
These changes in qua1tty of seismic record are j,n,terpre\ed as' a ll'eBu'Dt of those
w.!Lich
lbodk place in ,PeDetl'l8lted medium, and, most probaibly, as a resUllt of the changes l.n IdJthoal.ogy of ZechBtem. stzra.ta.. Mdteover, it ha& been f01.llllld that amplfitUidesOf.
sma.rrI elevaltiOlliS ma:r.ked on timeprorules - i.n the places of change of the chara.cta- of the Il"eOOl'd - deorea'Se along with depth. This seemsto
indicate the !PdSBi-bUJty cloocu:rranC$!
'of foSll'ilreer.
.InZec'hstem
depoeits.7. Poborskl J., Cima8zewski L. - Z
pa-leogeografii permu na Pomorzu. Dbidem, 1961, nr
'11.
8. P '0 b 0
r s
'k i J., Ma r
ek S. - Renesan'S poazu-,kiwati naftowych, na sbruktu'l'ach· ~olnyc:h regionu kujawskiego. Ibidem;: linO, nr 7... ..S. 'P r a c a 'ztrlorow~ - Ka.rbonatnYje porody. Izd. ,.Mlr". Moskwa, '1970. .". ". .. ',.
10. Zolojew T. M., Buor:owoj" A. M., Mied-w i e id i e w N. F. - 0 napraw'lenif poiskow za-letej gau w rifaeh lIlitniepierms'lrogo wozra'Sta siewiernoj bmtowoj zony Prlusp1jsk:oj wpad1ny. Gieologija Niefti i Gaza, 1170, nr 10.
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