Zbadane pr6bki pochocizllce :t porUUu romaflskie-go w Kijach pctLWolily ustalic, iZ do jego wykuoia uzy;to wapieni ze Skowronna; natomiast Ci08Y okla-dzinowe tego ~oiola wykonane zos-ta}y z wapieni sarmackich z Zyd6W1ka. Ponadto stwierdzono wy~ powanie wapieni z Kam:lennej G6ry w gotyckich
SUMMARY
The micropaleontological analysis was applied
as
a tool for identificati:on of the ,place of origin of the rocks used for architectural purposes. The results obtairied have shown that such approach may be useful for both restauration and studies of historical monuments. Moreover, the approach appeB.1"6 parti-cularly important in identifications of lithologically monotonous. rOcks such as LithothBlIDnium and bryo-zoan Tertiary limestones.
The procedure of rocks preparation for mJcropa-leontological studies is discussed in detail. Moreover, groups of mieroorganic remains applicable for rock identification are listed. The rock samples analysed were taken from fragments of architectonic monu-ments and various
deposits
of building rocks of the W6jcza - Piflcz6w Bange.. Some difficulties resulted frQI'D fragmentary rock material from arclrltectonic fragments, in comparison with vast amounts of mater-ial from quarries. Oceas-sionally, in the case of the lack
01;
roicrofauna. the analysis was carried out on the basis of lithological features of rock residu·um and by comparison with the re9Ults of petrological analyses C21'Tied outinde-pendently' by Dr. A. Bydzewliti of the Geological Institute, Warsaw. The results of micropaleontoIogi-cal and petrologimicropaleontoIogi-cal studies were also compared when the rock
was
too
hardto
free mieroorganisms. The PBIPer contains numerous photos of microfaunistic assemblages typical of different rook: types resem-bling the rock samples from architectural fragments. However, it sbould be stressed that not all themi-crofaurustie assemblages of rook samples from the arClhitectural monuments were found in samples ta-ken in the quarl'lfes. The final part of the paper deals with the results 01. micropaleontological studies of the rocks used for the conmrudfon of monumental buildings from the W~lica area, and a list of Ba-denian and Sarmatian rocks, tbe counter.parts of which were found in tihe field material analysed.
k~ciolach w Chotlu Czerwonym, Goryslawicach, W murach obronnych Wi§Ucy oraz w kamiemarce
Do-mu
l?Iug.osza;zU
wap.ien:l.z
Koperniuiyto,
mi~dzyfmlymi, do wzniesienia gotyckiej. kolegiaty
w
Wi-tUfey.PE3IOME
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