22. Wapien mal.'lglisty z detrytem, zbity i twardy (miejscami . przechodzi w margial), kremowoszary, frakcji troch~ grubszej, miejscaml. naloty tlenk6w manganu. W stropie tej partii konkrecje krzemieni czekoladowych; milliszoSc 1,70 m.
23: Wapien twardy, szarokawowy, z detrytuseru rzadk"o roz:rzuconym i UCZDll drobnll faunl4. miejscami przBkrystalizowanll, twarZ¥1l nagromadzenia; mblz-szotiC do 50 cm.
&PlS NOWSZ·E,T LlTERATURY
1. D m 00 c h I . - Jura qloezyfJs'ka. Acta geol. pol. 1158, V. VJII,IlI'
2-I. Bar c z ylt W. - Jura SulejDwa. Ibidem 11165. v. XI, nr il.
3. Bar c z y It W. - Ramlenlonogl z rodzaju Epltbyr19 z klmerydu oikoltc nty. Rocz. PTG 1985, t. XXXV. 4. ·D" b r 00 W B ,It a Z. - Klmeryd !Pod Utll. Blul. IG nr
19113. .
5. D .. 'b r 00 W B k a Z. - PrDfll warstw pognnlcza Jury
d kredy W Krzytanowt'CltCh pod. ruq. BluL IG, nr 105,
1911'7.
8. D" b row s k a Z. - The ·paueozolc and 1\Iesozolc In the $w!.t:to'k'rzysltle Mts. an<t the CalnOZDlc In the Car-pathlaon Fore<teep. Guide too Excumo.n Nil'. C 45 - Stra-ttgrapby of· the. Upper Jurasslc - Quarry Df Blazlny (1).
Wydawnlctwa Geologtczne. Warszawa 1988.
7. De m b 00 Wills: a J. - G6rna jura ml~ZY RalioonJe:m
a J~blem. BluI. IG, nr [953.
e.
K arc z e w <8 It 1 L. - SUmakl estartu 1 .1dmerydu.pM-·nocno-wschodnlego obN!ztenla G6r Swtt:toJtrzyltkl00. Pra-ce IG, 1980, t. XXXII.
9. K are z e W 11 k 1 L. - Stratygratla 1 fauna JJl8~ o1I:011c Radoms'ka. Blul.
ra,
nr 192, 19811.10. lK arc:z e 'W s It I L. - Rudlstae g6rnej jmy obrzetenla
G6r Swl~okrzy6klch (w druku) 1988.
11. K u t e k :t. - Kimeryd 1 bonon Stobnlcy. Acta geD!. !POl. 19«1, v. XI, !1'l' 1.
ll!. K u t e '11: .T. - G6rny JdtneI7d I dolny woJg p6inocno-..ozachOOnlego obrzetenta mezozolcznegD G6!' Swit:toltrzy-slt1ch. I'bldem il98l!l, v. XII, nr C.
13. K '11 t e Is: :t. - Krzemlenle 1 OBUWhika podmorskle w
dohlGII:!.Diet'Y'dzklch waplenlach okoUc Malogoszcza. lbl-dezn 1981, v. XI, nr .1.
14. Kutek J. Wlt'koowskl A. - Kimeryd 1 bonon z wlerced W ZaT~le. ltwart. gaol. 1963, nr -l.
15. 1\1 a 11 now s It a L. - Bloherma gllbkowa newtzu w
okotUy emte!owa. Blu!. la, m' IM, 19115.
18. 1\[ a 11 n'o'Wsk a L. - BIOIItratygratla do1Dego 1
trod-kowego okstOMU G6r Swlt:tOJtrzyllkteh. Blu1. IG, Ilr' 309, 1911'7.
17. 1\1 a 11 now 111 !I: a L. - Stratygratla mezozol1ru GOr Swl~DkrzyUlch. Cz~'(: - GOrna 'ura (w drukou) 1988. 18. P e 111 z a 't Cz. - Lttologia jura'Ulch ual ~anowyeh
rnl~zy Toltarnl" a C!rmle'lnlklem. Acta geD!. paL 1984, v .. X7V, nr 1.
19. Pellzat Cz., 1\Iorooz:-Kopezy:6s'ka 111. - 0 owyksztalcen1u Iltok!tr1eznym waplenl gOrno'urajoslklch na tpOI:udnle od Ch~cln. 'Roez. PTG. 19119, XXXVIII.
ZOo Pot a r y s 11: 1 W. - Jura ~ kreda o;llt:dzy Radomlem, Zawlchostem 1 Krainllklem. Blul. PIG, 11948, nr 48. 21. P.otarY'llltl W., Bleleoka W., sztejn :t.
--Stra·tygrafla mlkropa:1eontoologlczna ookollc Przytyk --~a pod Ralioinlem. BWl.
:ra,
nor 128, 19"'.211. P r a c a dJlorowa (pod red. W. Potar:r-sk1ego) - Prze-wodntk Wyclecllkowy N&1'aliy Patistwowej Shd'by Geo-IOff!czne' 1953 r. w,od. GeoI. 01953.
33. R a d w a ti tI \11: 1 A. - OIruwtska podmorakle vi malmle t eenonle mezozoleznego obrzd:enla GOr Swlt:tolkr:zySk:lch. Acta geol. lPoIl., 1980, v. X, nr 2.
24. ROt Y c 11: I S.
z. -
PaI'kln!lOnle, ganntlany 1stenoce-ra1l::l' z doueru obtzeienla GOr Swlt:tolkrzysklch 1 lch znaczenle stratygraflczne. Ibtdem 11155, v. V, nr 3. 25.
a
w I d z I ti oS It 1 H. - Kllka prze'kro16w przez l(6rnll'ur~ poludulowo-zaehodnlego zboc:za G6r !wlt:toJtrzy-.
s'klch. Prz. gecil.. ,tDn, a:r 9.
M. S a m fI 0 now 1 c z :t. - 0 %!otaeh krzemlenl w
utwo-ra.ch Jurajosklch 'POlnoeno-wschodn:lego IPibOCza 06r Swlt:-'tolkrzys'ki'ch. Wlad. areheo«.. 1923, VIII.
17. S a m son 0 w 1 c z :t. - Przeblejr I charakter granlcv mlt:dty
,ur"
a kred" 'Ila pMnocno-W5chadnlm zboczu~~6r. Slpra'W. PlO, 1932, t. VII.
21. S en 11: 0 W 1 e z E. - :fura I kreda mlt:dzy JelllrzeJowem a rzek" Nld4. Btu!/..
la
nr 159, 1959. .SUMMARY
The present opinions pn the lJiPper Jura-ssic of the mar.gi-n of the SwiE}tokrzyskie Mts. are given briefly, and the ~osures of the Upper Orlordian (" Astar-tian") and Lower Klmrneridgian found in the
north--eastern area of the margin are discussed.
The Lower Oxfordlan: Divesian and Neuvizyan, is fauIlIst£cally evidenced in the north-eastern an~
334
south-western margin areas, the Middle Orlordian~
Argovian, too. The deposi.ts of the Upper Oxfordian - "Rauracian" and "Astal'ltian" - developed as sponge limestones, and baIik: and coral limestones, disclose ample fauna of sponges, cora1s, bracb1opods and pelecypods, at places of cephalopods, partIcularly in the nol'th-eastern area of the margin, and so far have not been evidenced by ammonite fauna.
In the Upper Oxfordian quarries· at BIIa~ny (2 km south of nz,a, south-eastern margin of the Sw!~o
krzyskie Mu.) a complex: oc.curs of "Astartian" ·de-posits, cbaracterized by its special development. These are fonnations of Mypic reef. Here are found
antho-. ZOIans and ooMrf;es in compact, oolitic, ch8'lky anddetrital limestones, light grey and cream-coloured. Characteri'9tic fauna assemblage cOlllSists of thick-"Shelled pelecypodcJ (Diceras, Eodkeras, Pleswdiceras), gastropods (NeTinea, NerineUa), and brachiopods. In these deposits are found two horizons of flints, a part of which being syngenetic', othE!I'S epigenetic.
The Kimmeridian marIs and marlly 1Jmeston~, W'lth intercalations of lumachelles and shell limes-tones, are evidenced by ammon1te fauna. In the nol"th-eastern margin are found deposits of the whole Lower Kimmeridgillln, partly of the ~er Kimm.n-id-gian, Immediately C'Overed with the ValanginillI1 for-mations.
G6ra Zamkowa at IIZa reveals, at e:zposures, the Lower KUnmerigi'an fonnations, Immediately above the horizon Pktonia baylei. These are marts and marly limestunes, light grey and cream-coloured, with intercalations of Jumachelles and oo11te marls. The fa<UDa assemblage consists here of' pelecypod.s and brachiopods. EpithllriB subseUa (Leym.) and Epithvris cincta (Coflteau) are abundant, among pele': .cypods dominate MlIthilus (locaUy in ltmlachelles), Trigonia, Modiolus aeq'llliJp1iCatUis (S 0 w.) and Nanogira nana (8 0 w.). In the nOl'!1ih-we9tern area of the mai:gin,
in the vicinity of Tomasz6w, there occurs the whole Upper Kimrneridg'iQn, and its sedimentary continuity w::Ith the Portlandian, nemed by J. Kute4t - Vol-gian, can be obserVed. Here are found d~sl.tsof
Lower Portlandian and Middle Pol"tlandian age. The U!PPE!r Portlandian depasits developed in PUl"beckian :fiacies, are not found in the marginal area of the
Swi~akrzysktie Mts. The ne:xit area of their occurrence
is near PrzyItyk, NW of Radom.
PE310ME
B crarn.e ,lQae'l'lCH KJpaTJrnA oooop B3l'JI8,ltOB Ha Be,PXHlOIO ropy 06paMiJIeH'HJI OBeB'J.'olWIHC'lmX rap H
npH'BO,lVI'l'CS n:pMIIIE!PHLIe OIDfCamtII 06H~
Bepx-Hero ~All, "acTapTa" H HHJltH81'O KItII~a
cesepo-IBOCTO'UlOl'O 05pau:neHH.R.
HmK1fIHA OK~· - ,1\'Jme3 H HeBH3, a TBoICKe cpe',J\lHHA OK.CCPoP,lt - aprOB'HA OXa~OB&md
c1Jay-H'HC'l'H'IeCJKH B cesepo-BOCTO<IIfOA H ceBepo-3aD8)tH.OA
'1ac'l'.RX oOpaMneRH.R. IIOPOAhI BepxHeI'O OK:.ccpopp;a
"poplHI:a" H "aC'l'apra", npe,lI)c'I'aJunmH'hle r.y6g:OB&IMU,
paIIOOBHHHbIMH H Kopa.wroS&DtH H3Bec'llWIKaKH',
CO,ltep-:ata'l' fiol'8f1'YIO
<PaYH:Y
ryfioK, B1opgn~, mIe"IeBfOmXH lIen:eqmIO,lt, 3'Ha'D!TeJI&JK) MeHbWe ronOBOlHOl'HX;
ocOl6ea:Ho . B caeepo-llOCTo'lH'OA '1aiO'I'H 06pa.MJIeHHH, H ,l\IO owe: m>p He oxapaKTapH3OBaHhI Ha OC'HDBaIIDlJi:l aMMOHJi:I'l'OfB.
B ~ BapxseaKc<PoP~ dOPO.lt B
MeeT-HClICTM' Bna3HBLI (2 KM It ~ OT r. KmKa,
CeBE:!pO--BOC'l'O'Uloe 06pallJleHJi:le CaeH'l'OlOlIJi:llC rop)
Ra-6moA'QeTC.R IKOMDJIeJre nopo,lt "ac~apr.a", npe,ltC'1'aBJIE!IH-:
R&IX Xll!palt'l'epHNMH ,It.Jl'.R 3TOro RP)"Ca OTJlOEeHHIIDm
He'I.'JIlDAHOII'O. puq,a c ~K'Tall4'K !If OOJlK'TIlIMH. K HmI 0'1'B!0CRTCR: K.pE!IM'CIBEde H 'CBeTJIOCE!Ipide, u.ll!OrltiEde, OOJm'l'OOIble, Me~H)tR&Ie H o5nOM:O'IBDIe M3BeC'1'HHKK.
XaipalrrepHoe c1JaYRJt'C'.!'JAecJtOe coo6Iqecmo ~aB
o1Ieso mpyrrmop~ ne~· (Dkera.'1,
Eodiceras, Ptesiodkeras), op8XHOIl'OAaMH (Nerinea,
