12. Stolarczyk F .. Tyski S.-Warunld geolo-giczne ~wania ~owodor6w w osadach ordowiku i syluru syneklizy perybaltyckiej na tIe jej rozwoju. Ibidem, 1972, or 10.
13. 2 a r d e c k a D. - Sejsmiczne badania refiek-syjne w morskiej i lQdowej cz~/ici wyniesienia l..eby. '-Kwart. geoL, 1973, or 1.
SUMMARY
The 2arnowiec block structure is most distinctly marked in the Precambrian substratum and the Lower PaleoZ'Oic. This structure rises to the' east, towards the :f8Wt zbne 200 min amplitulk and NW-SE oriented.
On the basis of seismic data and !lri81.ysis of variability in thickness of sediments it may be assumed that the 2amowiec structure, related to the vertical movements of Precambrian substratum, began to differentiate already in the pre-Cambrian and in Cambrian times. A successive, more distinct stage of its development falls on th~ LUdlovian. Development of this structure was subsequen~y
accelerated in post-Silurian times, during I'lhort-term-ed (earliest Devonian) and much longer lasting (Late Carboniferous - Early Permian) phases of 4enud'a-tion of Paleozoic strata. vertical movements of sub-stratum blocks did not cease during the
ZeChstein.
The subsequent period of more distinct development of this structure falls on the Late Cretaceous and Tertiary times. An effect of neotectonic movements on the present form of this geological structure ofthe 2amowiec area is also observable.
14. ZbiOl'owa - SOwriemiennyje i nowiejszyje
dwiZe-nija ziemnoj kory
w
Pribaltikie. Pr. zbior. pod red. W. It. Gudelisa. AN LSSR. Oddz. GieografiiVllnius, 1964. ,
15. Z b i 0 row a - Budowa geologfczna syneklizy perybaltyckiej Cz. I. ,Pr. zbior. pod kier. S. Tys-kiego. Inst. Geol. - maszynopis. 1967.
PE3IOME
BJIOKOOOe CTPoeHHe CTPYXTyPbI )KapHOBe~ HaHeo-JIee' '1eTKO Bblpa'meHO B ,jpKeMopKAcKoM q,yH,llaMeHTe H B KOMUJIeKCe HKiKHero naJIe03oJt. OHa nOAHHKaeTcn K 3ana~, B 'HanpaBJIeHHH CfiPOOPBOH '30HbI, xapaKTe-pH3ytOrueHC$l aUDmfTy,n;OH ,IlO 200 MH 'npocTHpaHHeM
C3-IOB.
no
,n;a~ ceHCMH'IeCKHX pa60TH aHaJIHSapac-npe~eneHHH 'MOmHO('"TeH OTnOlKeBHH: -npe.!\IlOJIaraeTCH,
~ITO q,OpMHPOB8lmeC'l'PYKTypbI 2KapHosen; B 'wrore
BepTHKaJIbHbIX ' CMerul'mm: 6JIOKOB ;tlOIceM:6pIDi:cKoro q,YH,lIaJrreHTaHaqaJIOCb "erue B ~()KeM6PHH H npo;tlOJI-lKanOCb B KeKfipHH.CJIe~ll\ee, 60JJee 'ICTKoe q,op-MJqJoBaHKe 'CTPYKTYPbI npOHCXO;tlKJIO B 1fYP'JIOY H YCH'-JIHJIOCb nocJIe CHJIYP~CKOro 'oca~OHaKOUJIeHHH, BO BpeMS nepHO;DjOB ,I\eIIy;tla~HH naJIeDSOH: KpaTKOBpeKeH-Horo B'Ha'iaJIe ~eBOHa'H 60JIee DPOP'OJIJKHTenbHOro H CHJIbHOrO 'B HHTepBaJIe Bep~ itapOoH - BmKHJUl r.epKh. Bep'l'HK8JIbHhIe ~lifEeHH$I 6JIOJroB npo,IlOmKa -JIHCb H B :qeXWTeHHe. ,lJ;8JIbHmimee, fioJIee OT'IeTJIHBOe q,opMH,POBaHHe C'l'PYKTYPhI npOHCXO~HJIO B ' BepXHeKe-JIOBOe H TPeTH'moe BpeMs.He HCKJIlO'ieHO TaKlKe, '1TO Ha COBpeMeHHoe CTPoeHHe pailoHa JKapBoBe~ OK8Sbt-BaJIH BJIHID!He ,HeoTeK'l'OHH'IecjKwe ,~lifEeHHg.
