Niektóre parametry fizyczne osadów czerwonego spągowca monokliny przedsudeckiej

(1)

(2)

(3)

(4)

(5)

(6)

(7)

(8)

(9)

(10)

(11)

(12)

(13)

(14)

(15)

·468

.BUTKIEWICZ T., KOZłiOWSKA-KOCH M., PRZYBYŁOWICZ T. (11166) - Charak-

iIe!"ySt)'lka ~mna <Eadlrw' ^CDbl_ego ~ ze szczegól- nym uwzględ1lleDiml !plI/:wa .,... uziarnienia. Ar<:h. WG PAN (ma-

szynqJis).

wimrzawa. .

·CHlLINGAR G. V. (Jl9114) - Re1ationship belwoon po"",lty, permeabi4i1ty and erain-

slzo distrlbtitlion ol .anodo and sandston ... nevelopnenls In Sedlmen- torogy, l, II>- 71--8.1. l.dldon.

'LEVORSJ>N A. l. (1lJOO) - Tbe _ _ FIare SpeCe. Geatogyot petrol.,um. P. 93-

• 1(17 •. San F\nm""'oo.

:KARNKOWSKI~. (1'9'lI1) - PPer ... iIiP<ł<I1<ł<tt""ywy odkryc!a z!6t ropy _ i • _ u w ~

~il<ldmej Polsce. ~ geol., 19, p .. 1?!;-.l79, Ilr 4. W~a.

:KENT .R. E., WALMSLEY P. J. (!D'ro) - North Sao

pr_.

^{BuLl ..}at :AmErican

A109odlatlon ot PetI<ol<!um Geol~, 5&, IP- 167-ltll,. N9 l. Tulsa, Okila- homa.

:MIESZT ALSKI A, PODEMSKl M. (1l!7.21lJ - Zblle g""" w Grorl!Irlgen. Nafta, nr 4,

p. '1111)....,184. Ka1x7wIIce. .

.M1ESZTALSKl A., -PODEMSIKl.M. OI97.2b) - Zlote bituminów "" Ml<>nu P6l!nJoc-

nym.Na1'ta,"" 7, -p. ~.

KmawIIce: . . . . .

PODEMSKI M. (1970) ~ Smry ~ w okolicy NawejsalL. Klwurt. geol., 14,

. p.:im--.

~

3.

^W...--wa. ^. ^. ^.

. FlRŻYBYŁqWICZ T. 11008) - O ~ rozdzielenia cz.".~ 1 biMe80 "<P'I-

.~oa 'W ~ejanJie . CltrtrowB WieJlaapoJak:\ego na tle b8ld:ań p<>~ioz-

nych. Acta lIeol

PDI.,

^18,'Po 801~nr 4. Warll1'aw~.. . .'

:RUSSELL W. L. qw6o) -

. ResEnIain!_ ...-

1l'Oclr,s. Pl1Ioa!I>le<I ol.

lPdnileum

geaJ,ogy. p. 8Ih-116. New Yod<, Tarantlo, La>dan..

:RYDZElWISKI A. (111169) - iPl;b:_a:fli.a łuj:ji:Ów ";';_olinych <>echsztynu na mo-

.iok:liinie IpIr'Z<ldsIlclec;idel. Bill lmń.

G.iaI.,

^!li,^p. l1l:3-159. Wamzawa.

.SOKOliOWSKI

J.

ł!.9&'1) _ Cho!<8kteqtltJ!l<a ge.,~ • - - . . . . <lIlor<aru

przedstideciri.,gi>.,Geologia Budetlea,

a,

p.ll9'7-.'167. :W_zew ..

'V AN DER LAAIN G. (191lB) ..:... Phyoóoal

P1UPoJrlies

ot

i:h

e ~erVDlr and WIlume of

. . sas

liniItIally

iii.

!P~.

s,.".,.

^{!in _} Groo!fni'lll.1!Iis Ueld. Po Z&-&. Delft.

.DPĘD;I1!'łEHc;KAJ! H. C. (1970)-Oco6eJmOCTJl_1Hlll&:,OCtB ~o"""

ilOPOii """";i"ClIll

n_TCJ:I1l'Ol1POI1l6a

o.:rny6_ .HOB. ~. no

reoJi .

. He4JTel'II3. CCCP,.NiI 5, 0Tp. 36--39. MQOJ:Ba-JlmDiBrpap;.

:llPODllJJIKOB E. K. 0960) ---: 3aB1SCII'MOCTJ, .EO~ CBOlIcTB QT rllY6HB>i 3&lJtii'8BlIlI 1/ mtrolIOIli'ieClroro 00CT8lI8 _ .

reoJionur aetnr

^1/^.I'Il3I.,^{HI 12,}^CTp.^24-29.

Mooua.

JIPOmJiJIKoB E. K. (1969) - HOBOe B

..,ro_

^0I\CBDłKOJDIerrOpoDXClIClIIc1l. TOppIIi"eH-

""'" IiOPOii. Hc:4>rera3oJl8l[ reolIonIJI 1/ r~,.NiI 8, OIP.

40-4,.

^Mocna.

(16)

Str .. zmenle

469 AlweiI

MEDITAJIbCKlł

HElCOTOPLlE 4I1ł3Jł1łECICIfE IlAPAMETPLI KPACHOro JII!lICHIIIlPE,l(Cl'ĄETCKOA:

·MOHOlCJIHHAJlH

PeSIOMC

C Il<lI!dO YTO'm''''HII "PIttCpJteB 0l\C>I!K1< llI3OHOCHocTK cepIOl "POCHoro lI<ZIIll Ha n _ - cy,l(e1'CK.Oa MOHOXJIJiBaJDt npoB3B~ ,u;eT8.1lloBl.Ilł aB8JIIitł BCeX ,IJ;OC'l'YJIlll>IX ,IJ;B.lIB&1X, onpe,JJ;eJlI:·

~ 4ntDt'Iecme CBOJłcTBa J:OJI.IIC:I:I'OpcDtt roplł3OBTOB 3TliX OTJIOICBldł.

OcooBOlt :mIX ~BaJUiII

.o"""""

peoym.TaTr.I na6opaTOpIlWX H3IIepOmdI ~ aop~ B .apoR1IQ8e:LfOCT1t, pe3ym.T8.n.t IJpOMLICJlOBOI

reoctntnmK,

0IXI'k:aIQiI: IepBOB li. IWl8M8.,

peoYJII>TaTW lXeTPorp~ _olllUD!l, a 7ana> 110lXO~ ~ ~K

TJiBBoI: UopliCTOCTK B epBBX, DpO~ u:ycl'JilłeCK:ltM MCTO;o;OM.

Bwm~HH>l. ,I\IUDłIole llOOIIOllIlIIH ""'J\ClIIITl> B _ " " " " "JlII"lloro lI<ZIIll llpeJ1cy-

~o:l: MOHOKJIlDl8JJ1C J:JeCUIIYIO cepIDO, MOJltBOC'Ilt,lO ar BecIOJIhDIX NeTpOB .QO cswme 400 M, 38JIeI'8lOIIQ'I B :qKlJem,BO:lł 'i8.Cllt pa3pe38. BltmIe:Ił: IJCpMB. B CTan.C OHA ycnOBBO B8!1B8.B&

,,no~OBO:łł: JJeClIaHo:lt cepJreA: EPacHoro JIemDf'. B 3TQ:It cepmr, r,llC cpaBmrrem.HO nono oro6paa ICpB, npo:ae.u;eHO ,llOCTS.'f01IBoe K.OJJlflłeCTBO IlIIII1IB3OB ~0B8BB&IX Il8.paMeTpOB.

0lDt co6pam<, 1 1 -li ,I\01'BJIhIłO IIP""BauE!tpOlIIUUl B COIlOCI1IBHOIIH C lIlIpOTaJDI>DUł KJ)JOl&JMIt, a 38.TeM yCpC,zr;HeB:W DO ~oł. C!pa'ERB'c. Yc~eHIIHc Be.IDNIiB:Erl: 34Jc1kantBHol:

DOpJtcTOC'I'Jl Ii npom.tr:taeMocm ~oI: ccplilt, ee MOII(HOCT,H ltrpy6mm!38lIelaBJiJl ~

B T8.~ H ynol'pe6JIeBl:iE AM COCTBBJIeKU ,n;Barp8MM, B ~ ycniBoBnCBBI: liX B3BlDd:O"

3alIlICIIMOCnI

(.pr.

I-S).

Pmy_T&TJoI, nOn;yftB:HWe lD yn3'RBNJ' ,ItIl8IpBMM. BMeCTe c COC'I'8.BJJeBBO cxew.ałt K30IIaXIIT Jił B30T0lX

(.pr.

6) _oBamrolI cepu MOt'yT lIBlIllT>CJI BIIZInoIM:>JJeMeBTOM up. o_enemm

.A8JI&Be1łrmIx B8IIp8.BJICIIld DOJJCJ:OB yrJICBOl(OpO;o;OB Ba ODKCf.łB8eMOA TelJPBTOplJJ!.

SOME PHYSICAL PAJlAMETER8 OF TBE ROTLIEGIINDES IN THE FORE-SUDETlC MONOCLINE

Summao:y

:In <11:<1 ... ID d_e 1ibe e.riJt>eria oli' ~'IliI01IiIlg the _ "",,'bent ol the Rotliegendes seri ...

wt_

>the Fore.sudEolie monocllne area acclll"ately. a detalJed ana!ysis has been mede ol en avft'lilollle dalia

_t

determl.noe !be physicaJ. ~..

at

!he r .. ervolr horizons

at

the period. These inveo'Ugatlons have been Ilased on !he ...w.1B 'Ot labocaltx>ry m...,....,...ts of ettectIve ~ amI permeabiJ;fJty, the results of bore-hoie geophy:sllca! surveYB. _ descrf,ptiXQ

at

drill 00ftB and O'f drl!l

wttIn!is.

*he ... ts of ~ examblltIoos, aDd .tf1e

<XmIPI-ta-y

mEOIIRI1"emen1B lOt ef>!edłive pcmJSIty. maxIe usIq lHl<l<l8tk metbod ClI1 dl'lll1 001" ....

'!'he ebove data a1lowed 1ibe _thoor to ~h, _ Jthe Rotl>eg.,.,des formations of t:he F-ore-Sudetic monooline,

an

arenaeeous sedes ranging in thickness

!mm seveni! 'In "",,*ellban 400 metres.

new",'y

00CUl'<"iIlg at iIbe top pori:Ioo ci Ule

Streszmenle

469 AlweiI

MEDITAJIbCKH

HElCOTOPLlE 4I1DH'1EC1C1fE IlAPAMETPLI KPACHOro JII!lICHIIIlPE,l(C'Y~OA:

·MOHOlCJIHHAJlH

PeSIOMC

C Il<lI!dO YTO'm''''HII "P1ttCp1teB 0l\C>I!K1< llI3OHOCHocTK ceplDl "POCHoro lI<ZIIll Ha

npejl-

cy,l(e1'CK.Oa MOHOXJIJiBaJDt npoB3B~ ,u;eT8.1lloBl.Ill: aB8JIIit) BCeX ;o;OC'l'YJIlll>IX ,IJ;B.lIB&1X, Onpe,JJ;eJlI:·

~ 4ntDt'Iecme CBOJlcTBa J:OJI.IIC:I:I'OpcDtt ropll3OBTOB 3TliX OTJIOICBldt.

OcooBOlt :mIX ~BaJUiII

.0"""""

peoyJlJoTaTr.l na6opaTOpIlWX H3IIepOmdI ~ aop~ B npoR1IQ8e:LfOCT1t, pe3yJIbT8.n.t IIPOMLICJlOBOI

reoctntnmK,

0IXI'k:aIQiI: IepBOB Ji. IWl8M8.,

peoYJIhTaTW IXeTPOrp~ _olllUDll, a 7ana> 110IXO~ ~ ~K

TJiBBoI: UopliCTOCTK B epBBX, DpO~ axycTJiIIeCK:ItM MCTOAOM.

Bwm~HH>l. ,IIIUDIIole IlOOIIOllIlIIH ""'J\ClIIITl> B _ " " " " "JlII"lloro lI<ZIIll llpeJ1cy-

~o:l: MOHOKJIlDl8JJ1C J:JeCUIIYIO ceplDO, MOJltBOC'Ilt,lO ar BecIOJIhDIX NeTpOB .QO cswme 400 M, 38JIeI'8lOIIQ'I B :qKlJem,BOI: 'i8.Cllt pa3pe38. BltmIeI IJepMB. B CTan.C OD ycnOBBO B8!1B8.B&

,,no~OBO:l JJeClIaHo:li cepJreA: EPacHoro JIemDf'. B 3TO:It cepJDr, r,llC cpaBmrrem.HO noJIRO oro6paa ^ICpB,npo:ae.u;euo ,llOCTS.'f01IBOC K.OJDfIR:CTBO IlIIII1IB3OB ~0B8BB&IX Il8.paMeTpOB.

0lDt co6pam<, 1 1 - • ,I\01'BJIhIIO IIP""BauE!tpOlIIUUl B COIlOCI1IBHOIDD C lIlIpOTaJDI>DUl KJ)JOl&JMIt, a 38.TeM yCpC,zr;HeB:W DO ~ol. crgaEH'Rc. Yc~eHIIHc Be.IDNIiB:Erl: 34Jc1kantBHol:

DOpJtcTOC1'Jit Ji npom.tr:taeMocm ~oI: ccplilt, ee MOII(HOCT.H ltrpy6mm!38lIelaBJU: ~

B T8.~ H ynol'pe6JIeBl:iE AM COCTBBJIeHU ,n;Barp8MM, B ~ ycniBoBnCBBI: liX B3BlDd:O"

3alIlICIIMOCnI

(.pr.

I-S).

PmynT&TJoI, nOnyftB:HWe lD yn3'RBNJ' ,ItIlaIpBMM. BMeCTe c COC'I'8.BJJeBBO cxew.att K30IIaXIIT lit D30T0IX

(.pr.

6) _oBamrolI cepHH MOt'yT lIBlIllT>CJI BIIZInoIM:>JJeMeBTOM upJi o_enemm .A8JI&Be1trmIx B8IIp8.BJICIIld DOJJCJ:OB yrJICBOl(OPO;o;OB Ba ODKCN"MeMOa TelJpBTOplJJ!.

SOME PHYSICAL PAIlAMETERS OF THE ROTLIEGIINDES IN THE FORE-SUDETlC MONOCLINE

Summao:y

:In <11:<1 ... ID d<'fine 1ibe e.riJ\>eria

at

~'IliI01IiIlg the gas "",,'bent of >the Rotliegendes seri ...

wi_

^>theFore.sudEolie monocllne area acclll"ately, a detailed analysis has been made cl an avft'lilollle daJIa

_t

determl.noe the physicaJ. ~..

at

the reservoir horizons

at

the period. These inveo'Ugatlons have been based on the

...w.m

'Of labocaltx>ry m...,....,...ts of ettectIve ^~ami permeabiJ;fJty, the results of bore-hoie geophy:sllca! surveYB, ;the descrf,ptiXQ

at

drill 00ftB and of drl!l

wttInIis,

the ... ts of ~ examblltIoos, aDd ·tbe

<XmIPI-ta-y

mEOIIRIl"emenm lOt ef>!edtive pcmJSIty, made usIq IHl<l<l8tk metbod ClI1 dl'lll1 001' ....

The above data allowed 1ibe authoor to ~h, _ Jthe Rotl>fgmdes formations of the F-ore-Sudetic monoollne,

an

arenaeeous series ranging in thickness from seveni! 'In "",,*ellban 400 metres, newarty 00CUl'<"iIlg at iIbe tap pori:Ioo cl Ule

(17)

470

Lower PermOon dęx>sIts ,peneb:lated. In the IPM!eDt ... 1:iclethis ~es .. tenta.t1ve1y ca.lIed '\!he Sub·Zecbstdll arena.ceous Bel.'lies ot IWtlieg<model". Ofthis ser! .. , rela1i.

v:e!ly weE. penetrated and with a high core lre!OOVB'y, a lot ·al parame'bnes have been

<maIysed. They Ileve beon gatbered, ocm>p1eted, """"",,,tely ...uysed 011 tbe basIa o/.

Jogging data, and then &veraged for each drllUng. The average resu11ls <Jf effectlve pot"<lIrlty md perme8bll!Ulty ^dfll"<loCka ot the Sub·ZecilJ&Itein arenaceauB s _ ot ^RotLle- gendes, 18& well ... :As th1dmJ elSse:s and oOfXW:'.retl'Oe deptils

_e

^preeented^.in^{Table 1.}

'1'bese data mve been Ule<! far coostructlon ot dlognunS ^ÓIIlorder OC> enplain thElit

rela_ips 1(FI8s. l~). .

The resuJta obtained ,trom the abave diagrams ean be, a\ong wit;, the isapacbyte a.nd ;"qpor slre1lch ot ,the s _ uruIar exammat.i<lln (Fig. 6), "'" lmporibant ekment dUl1iiDg determilinabiun <lff fur·th.... doirectia1s in """""h far hycIL""",1xca! with.in 1IIIe area <>JIl&'k!eooed.

470

Lower PermOon ~ts ·peneb:lated. In the IPM!eDt ... 1:iclethis ~es .. tenta.t1ve1y called '\!he Sub·Zecbstdll axena.ceous Bel.'lies of IWtlieg<model". Of this ser! .. , rela1i.

v:e!ly weE. penetrated and with a high core lre!OOVB'y, a lot ·af parame'bnes have been

<maIysed. They Ileve been gatbered, ocm>p1eted, """"",,,tely ...uysed 011 tbe basIa 01.

logging data, and then &veraged for each drillIng. The average results <Jf effective pot"<lIrlty md perme8bll!Ulty of ll"<loCka of the Sub·ZecIh&Itein arenaceauB . _ of RotLle- gendes, 18& well ... :As th1dmJ elSse:s and oOfXW:'.retl'Oe deptils

_e

^preeented^.in^{Table 1.}

'1'bese data mve been used far coostructlon of dlognunS iIin order .., enplain thElit

rela_ips i(FI8s. l~). .

The res\Jlta obtained ·from the above diagrams can be, along wit;, the isapacbyte a.nd ;"qpor slre1lch of ,the series uruIer exammat.i<lln (Fig. 6), "'" lmporibant ekment dUl1iiDg determilinabiun of fur·th.... doirectia1s in sea:r<lh far hycIL""",1xca! within the area <>JIl&'k!eooed.