Wyniki wiercenia Lublin IG-1

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+NQ~ ____________________________ ~~~L-______ ~ ________________________ ~ m +200 -0 -1000 -2000 -3800 B 10 k Wilczopola ·U. -1000 I Q' P . a d ( i s k 0 -3000 Irazimierzowki -4000 \ -________ ~---____ ~D.~~ ______________ _1~0 -JOOO

o

I . - I _ _ _ _ ....!. "firm

e

przecif:cie ,taszezyzny fYzekroju przez oIwrSr lublin 161

~ powierzchnie denudac!Jine

Ryc. 5. Przekr6j geologiczny B - B.

malnych) war6twy w zapa·dolisku K'8zimi~rz6wki

za-padajll w ikierunku uskoku Majdanka.

- U&koki wyst~pujllce tu, a b~q<:e wieku astu·

ryj-skiego nie ,przecinajll calego kompleksu,' a ulOiZo.ne

klllisowoograniczac si~ mogll do cz~ci profilu

obej-lID.uj~cego jedynie d~won lub .kamon, cz~iowo' tylko zaburiajll'C caly ten kompleks.

IPoda.ne powyiej wnloski dotYCzllce obrazu

prze-strzennego przedstawio·no na szkicach stI'ukturalnych

i przekroja·ch.

LITERATURA

1. lDayczak-C.alikowska K. - Uwagi w

spra-w.ie stratygrafid OBa·d6w jury ~rodkowej mi~y

Garami Swi~tokrzyskimi a Bugiem. Prz. geoI:

1965, ·nr 2. .

2. Le w i fl s kI J. - Jura w gl~bokim wderceniu w

Lu'blinie. Posledz. ,nank. Panstw. .!nst Geol. HI33,

t. 35.

3. MHaczewski L., Zelicbowski A. M.

-iWgl~na budowa geologiczna obszaru radom6ko--luibelskiego. iPrzewodnik LXII Zjazdu PTGeol. 197.(). .

4. Ni e m c z y 0 kaT. - Stratygraofia ok.sfocdu cen-tralnej Lubelszczyzny w powillZaniu z pro-filowa-niemgeofizycz.llYm otwor6w wierbniczych. Kwart. geol. 19'ro, .n·r 2.

-5000

Fig. 5. Geological cross' section B - B .

... Soko·lowski J., 2:elichowski A. M.

-.wst~pne illiformacje 0 wyst~powa'niu gazu

ziem-nego

w otworze Lublin IG·d. Geofiz. i Geal !Ilaft.

1968, rir5-.6.·

6. 2 e I i C' h 0 w·s ki A. M. - ZaI'Ys budowy

geolo-gIcznej iLubelskiego' Basenu Karbonskiego. Prz.

geol. 1004, m' lil. " .

7. 2: e 11 c h o'W S. k i A. M .. - Stan ;rozpoznania

wgl~bnej budowy geologicznej Lubelszczyzny. Ibi-dem, .1970,

.or

9.

SUMMARY

. Within the area of the-Ce.n.tral Lublin Region, .in the central part of the YOWlg Palaeozoic foredeep

zone,a deep bore hole LubYn IG-Il has been drilled

by the Geological EntelWI'ise

to

the order of the Geo-logical Institute, in 1'966-1968. At a depth of 5028

m

the Lower Devonian formations were found, develo-ped in :the Old oR~d Ifacies. The section is as follows.

Quaterp.ary deposits (0-1 m) are underlain with

marls, opokas and· limestones of Upper Cretaceous age (depth -1-:-623 m). Jurassic for·matio.ns (823-102'8

m) a're represented by marly limestones and

dolo-mites ofK..immericigian age (67 m), by oolitic and

detritallimest,ones of Oxfordian age (133 m), by are~

(7)

Bathonian (6fJ m) age. TIbese r-est on the Car,boniIte-rous depOSoits (depth lloos--.al68 m). The CarboDHeCar,boniIte-rous is represented by the deposits of ,Westpballan ;A (2M m), iNamurian (602 rn) and Upper Vi1renian

(:US,6 rn). .

Il'he

Devonian formations (2138-6028 m) cOll9is't of calcareous-mady deposits of Famenman age

(l4:i8 rn) and coralUne limestones of Fra&nian age

(300 om), as well as of car'bonate-&nhydrite limestones of Givetian age '192 ro)., and anhydl'ite-a!L'enaceous lime&'to.nes of Effelian

m

age IQ230 lID). The Lower [)e-vonian is ,built

o:r

soiItstones and sandstonea cif Old

Red type (more than 130 m). Due to the .considerable dftps, the thiclmesses are given i,n ;reduced values. The bore hole has been deviated during drilling acti-v.tty about

.wo.

Some fault zones have been ascertai.ned dtu'ing

the drilling process. The madn fault bas been milled through ai an interval of about 4600--4800 rn, and the bore hole has entered a separate tectonic block (Figs. 5 and 6). The .bore hole ,is situated, as it :results from the ·mterpret.ation here presented, in a marginal part of a nar.row iforedeep, the SW fault of which represents a .normal fauli, whereas the remaining ones resemble antithetic faults dipping in ,its direc-tion. This foredeep was formed dlB:'ing the deWlop-ment period of the Mazowsze-LubUn graben, at the Asiudan orogeny .time. [lisloca'tions alder than those ones reveal diabase dikes. A dike found to occur within the Famennian .deposits .Is, aocor.di.ng

to

the age tietermination lIIlade by T. ~uch at the

Geo-logical Lnstitute !by meB'llB of 49 IKr~40Ar method, of Lower CarboniferoUoS age (333 miH. years).

PE310ME

B ~eH'11PSJILH'OA 'IacTH JIro6J1HBCltoro perHOBa, B

30He 'BepJMeIIaJle030AcKOro nporH6a B 1966-68 rr. 6hIJIa npoA~eaa rJly60KBJI CKBBEHHa reo.nol'H'lecJtOro

JIEIC'1'IS'1'Y' JIlOOJnftl Hr-I. OHS ~JIa rny(lJUlLl 11028 K H 6hIJI8 OCTSHOBJIeHa B DOpOAax HJOItBel'O

~esoHll. Pa3pe3 6ypoBOA CKBaEHHhI npe~C'l'8BJUleTCR

CJI~~ 06p83011:

q~ OTJlOEemm (0-1 M) rrOAC'llHJIaIOTCSI Kepl"eJII.Df.H, OIIlOII:8l1Dl n n:mec'l1HHKa1m: BepX'Hero MeJla

(KH'l"SPaaJI 1-823 M). IOpa (823-1028) ~aBJleH8

MepreJIHC'l'LlM'H Jl3Bec'l"HJUt8MH IK ~OJlOM'H'l"llllm: l!Xl\Ile-PH'.IPKCKiOI'O HPyca (67 M), OOJ1'HTOBLIM:K 5t o6JroMoq-m.nm Jl3BecT.mmal\m OlrecPop,zta (133 101),

Uec'laHH'C-TLIMH H3Bec'.l"lmK'mm KeJlJlOBeSl (9,5 M) n BeipXHero

58m (5,5 K). IIo~ IDDGl 3aJleraer Kap60a (1028-2158 aI), npe,!tC'NIIBJIE!RHLrli rropo,ztSlm Bec'l'$uIB 'A

(224 111), muuopa (502 M) H aepXHerp BH3e (318,11 K). K ~eBOHY (2138---fi028 M) OTHOCJITCB

JC3BecTKOBO--Kepremt;C'l'J:ole IJopo.ztLI cP8.KeEla (1458 K), KopaJUIOBbre JC3B1!JC'l"BJIDt cPpaBa (302 K),

Kap6mUl'l"H()-alJl'HAlPHTO-BhIe H3BecTH.BlDI :atHBerQ (192 K) H ~nec'la

HHcTI>Ie H3BIl'C'1'!Iim:H 9Aq,e.M? (230 101). HmKmdt ~eBoB

IIPeACTSBJIeB aJleBpomnoaMH H nec'lamm:aMH oJI,JU>e~-CIroro 'l'JI[[a (cBLIIIIe 130 K). .

'YrJlLI ll!8,II;eHJm CJloea O'leHL KPYTLIe, B CBR3iH C 3'l'HM YKa38HIBLIe M~OCTH 6LIJl1H COB:p8IIlem.I. B

n:po~ecce II!pOXOAKH CIm38J1ml1a O'l'K'Jl'OlDfJ1'aCh no

a3H-J6yory OltOJlO 40°.

B P83.pe3e aKBaJItHBLI Ha6JIro~aJlOCL HecKOJlLKO

cfjpocOBLIX 3OH. rJlamn.rll clSpoc 6hIJI nepeceqeu B

HHTepBaJle 4600--4800 M. HmKe 9'1'01'0 JfH'l'epBSJl8 ClJCBalKHHa BCJq)blJIa a:aaLUi: TeKTOHH'leclOdl: 6J1OK

(4nn'.

5, 6). CorJI8'CHO IJP()Be,JteBHOA ~,

C'KBaJKHHa Jbo6mm Hr-I pactl'DJIaraeTCB B Jtpaesmi

'iSC'l1K y3B.'Oro npom6a, B KO'l'OpOIoI c6poc,

orpaHH'IH-BaIOIl\d

ero C 1Ol'(>o3aIr8,zta, KMeel' IIOPMaJILm.di: Bn,zt,

. a OCTaJILHhIe c6pOChI aHTH'l'e'l'H'IecKOro xapaKTepa H8K.lIOHeBLI It HeMy. IIp0rH6 00p83OBaJICB IJpH q,op-MJfpOB8H!HH JII06Jl1HHCKo-Ma3oB~oro rpa6eHa B ac-Ty,pJiA'cltOA q,a3e. K 60JIee ,tUleBHHM .zt;HCJlO~ npHypO'IeHId .ztH'a6a3OBhIe ,ztaAltH. ~iiKa cpe,ztH

cPa-iIleHCRlHX napo~, npo~eJmBJI CKBaEHHoA, no

cmpe,ite-JlemIJO T. ,ZI;ecqroxa MeTO~OIM 40Kr'40Ar, O'l'HOCW1'CSI It ltap60uy (333 KJIH. JleT).