28. S t u p -n
i
c k a .E. - Wykorzysta-nie Ibadan prze-,prowadzonych w poludniowo-zachodnhn obrze-zemu G6r Swi~tokrzyskich ella prac poszukiwaw-czych ·na lProzedg6rzu Karpat. iNaita, 1970, nr 11. 29. Z nos k 0 J. - Problemy tektoniczne obszaru pozakarpackiej Polski. Prace Inst. Geol.t.
30, cz. IV. 1963.30. Z nos k 0 J. - Problem kaledonid6w d gra.nicy platf.ormy prekambryjskiej w Polsce. Biul. Inst. Geol. 188. 1965. .
31. Z nos k 0 J. (red. nauk.) - Atlas Geologiczny ·Polski 1:2000000. Warszawa 1968.
32. Z nos k 0 J. - Pozycja· tektonicz·na obszaru Po1ski. Biul. lnst. Geol. nr 251. 1970.
SUMMARY
The Palaeozoic core o.f the Swi~tokrzyskie Mount-adns 'is surrounded with the Mesozoic and Tertiary deposits (E'ig. 1). A lack of Mesozoic formations w.!thin the area of the Palaeozoic core is due to the post-cretaceous erosion, since the Swi~tokrzyskie Mountains run just at the axis o.f the pericratonic trough filled
an
with the Mesozoic deposits, some kilometres in thickness. Thus the thicknesses of the individual stratigraphic members' increase, going from the -north-east and south-west to the Swi~krzys'kie Mounta!lns (F,ig. 2).
The post-Cretaceous vertical movements of the Earth's crust were of complicated nature. At first, at the post-IMaestrkhtia.n time, the Middle-Polish rampart arose a'long the pericratonlc tl"ough, and
then,
parallel to the Carpathian geosyncline, an element uplifted, called by the authors the Meta-Carpathian Arch. Su~equently, ttlUsarCh plunged UJIlder the Oarpathian overthrust and the Csrpathian fore'deep. The SWi~tokrzyskie Mountains are a fragment of the northern slope, which was not lowered at the Neogene time, of a large dome for!Ded in ~he Pala-eogene at the crossing of the Mlddle-Pol1sh swell and ofthe
Meta-Clll'Ipatianzone.
The Middle-lPormh !raln!pari WIllS formed aot the axis of a subsidence in the pericratomc trough which la-sted through the whole Mesozoic time. The Meta--Carpa-thialll A:ch. ,was, fin turn many times uplifted in the Alpine diastrophic cycle, and in consequence
of this dt !is charactel"'ized by smaller tMeknesses of Mesozoic deposits than the Middle-European
syne-clise situated more to the north.
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