• Nie Znaleziono Wyników

Przesłanki dla poszukiwań złóż dolnodewońskich piaskowców kwarcytowych w rejonie Iwanisk

N/A
N/A
Protected

Academic year: 2021

Share "Przesłanki dla poszukiwań złóż dolnodewońskich piaskowców kwarcytowych w rejonie Iwanisk"

Copied!
10
0
0

Pełen tekst

(1)
(2)
(3)
(4)
(5)
(6)
(7)
(8)
(9)
(10)

7. Tar now s k a M. - Wynikl ilo~clowej analizy lltologicznej i korelacjl dewonu dolnego w :regio-Die kieleckim. Kwart. geol. 1971, nr 2.

8. Tar no w s k a M. - Dolnodewoilski.e skaly po-. limiktyczne i tufogeniczne w regionie kielckim

G6r Swi~tokirzystkich. Ibidem, 1971, nr 3. 9. U r ban ski A., W a c how i c z Z. -

Dokumen-tacja badan geofizycznych dla poszukiwafJ. zl6t piaskowc6w dolnodewonskich w rejonie

lwa-SUMMARY

The paper deals with preliminary results of pro-specting and Uthological and raw material studies of

Lower Devonian sandstones from the Mea of lwa-niska. On the basis of historical, geological and geo-physical premises it can be assumed that ~ the area of lwaniska a number of qUB!'tzitic sandstone depo-sits OCCIll' in the vicinity of P~ba G6ma, Podlesie and Kopiec. FavoUll'able conditions for occurrence of the sandstone deposits exist in zones of transversal depressions, where the Lower Devonian attains grea-ter thickness and where the belt of its outcrops is much broader. (Fig. 2).

The scheme of lithological-facial development of the Lower Devonian, reconstructed by the author, is very useful in prospecting for a:aw material depo-sits. The profile of the Lower Devonian consists of two mottled series sepaa:ated in the middle by a sand-stone series. I"ocally, there also OCCUll' thin upper sandstone series. Quantitative llthological analysis showed that only the ntiddle sandstone series of the Lower Devonian, which in the depression zones of

POll'~ba G6rna and Podlesie is up to ,50 m thick, re-presents a deposit value.

The occUll'rence

at

deposits of Lower Devonian sands tones in those regions is also confirmed by the results of electroresistance and geophysical logging surveys. Geophysical characteristics of· the Lower De-vonian in the area of lwaniska have been elaborated (Table I). It has been established that. the middle

sandstone series, interesting as a deposit, has con-trast geophysical pa:operties in relation to the

adjoin-ing mottled series. Correlation of electro-resistance curves with geolOgical pa:ofiles is remarkable (Fig. 3). Usefulness o:f electro-resistance surveys was ,found both in prospecting and documentation od: deposits of Lower Devonian quartzitic sandstones.

Favourable physical and strength properties of the sandstones point

to

their wide applicability in general and engineedng building, in road and rail-way track building, as well as in production of ag-gregates and semiproducts (Table Ill).

Disk w G6rach Swi~tokrzyskich. Maszynopis, 1972, lG.

10. W rOb 1 e w ski T. - Charakterystyka geolo-giczna

l

technologiczna .,kwarcytbw" i piaskow-cow kwarcytowychG6r Swi~tokrz,yskich. Maszy-no pis, 1971, IG.

11. W 11' 6 b 1 e w ski T. - Geologiczno-surowcowa charakterystyka piaskowc6w kwlU'cytowych w

G6rach Swi~tokrzyskich. Kwart. geol. 1972, or 4.

PE310ME

B pa60Te npe~CT8B.JIeHbI npe~pHTem.H.Lle· pe3ym.-TaThI DOHCKOB

n

JIHTOJIOrO-TeXHOJIOrn'leCKOrO HCDhI-TaHJUI HKEH~eBOHCltHX IIeC'l8.HHKOB pm!:oHa l'lBa-IlHCKa. KaK MOEHO CY~I1Th Ha oCHoBaHHH

J'lCTuYlhc.c-KHX cBe~eHJdl:, a TalOKe reoJIOrmeCKKM

n

reoipH.:$J'I-'ieCKHM AaHHhUd, Ha J'lcCJIe,z;;oBaHHoii nJlO~Wf MlIII .. ",·l'Ol.

MeC.lWJU:dCO 38JJe:m:eA KBapL\J'I'l'OElhIX neC':llutw<oa, 111£"-nOJIOlKeHHhIX B paAoHe MeCTHoCTeA I1opeMtla-l'ypHa, lJ.oAJItce H .l\.one~. b.naronpnaTHhIJrU:! 30~aMJ'I pa"u}.lO-CTpaHeHJm 3aJIeJKeti neC'laHHKOB SBJIJIlOTCJI aOHhl no-nepe'lHhIX nporJ'l6oB, B KOTOPhIX HJflKuHA ~esoH

06-JIa~aeT IIoBhImeHHoti lIIIOIItHOCThIO H ~aeT KPYIDihIe

BhIXO,J.{hl (qna'. 2).

BCUKHoe 3Ha"leHHe ~JIS nonCKOB paCCMa'l'PJJBaeMbIx none3lllolX HCKonaeKhIX HMe.na COCTaB.JIelmaa aBTOpoM cxeMa JIHTOJIOro-cpaqnaJIhHOrO pa3BHTJm lUDKHero ~e­ BOHa. Paspe3 HHlKHero ~eBOB8 COCTOHT H3 ~ElYX De-CTPhIX KOMIIJIeKCOB, pas~eJIeHlihlX cpe~HKM nec"laHH-KOBhIM KOMIIJIeKCOM. Konn'leCTBeHHl>Uii: JIH'l'OJJOrH'IeC-KH1l aHa.JIH3 IIOKa3aJI, 'lTO npoMhI1llJIeHHoe 3fta'leHKe HMeeT nHIlIh cpe,lUiKll IIeC"IBHHKoBh11i KOMIIJIeKC HKE-Hero ~eBOHa, ~OCTm'81O~ B norpY:m:eHIlbIX 30dax B pm!:OHe MeCTHOCTeti nopcM6a-I'ypHa

n

1I0~JIece bO M M01ItHOCTH.

PacnpoCTpaHeHHe 3anelKeB: HmKHe~eDOHCItHX IIec-'1QHHKOB B 9THX paitOHQX nOp;TBep1K~QeTC8 TlUOKe p;aH-HhIMH C'hel\UW MeTOAOJ( 3JIeKTpOCOnpOTmmeHHil:· K reo-q>H3meCKOro KapOTalKa. COCTaBJIea8 reoq>H3H'IeCKaa XapaKTepnCTKXa HmKHero p;eSOHa B paifoHe MBaHHCKa (Ta6JI. I). KOHCTaTHpOBaHO, "ITO cpep;mm lleC'laHHltO-BhIti KOMIIJIeKC O'l'JIn"laeTCS KOHTpacTlUoIWI reolPH3H-'1eCIGDm CBO~CTBaJom DO CPaBHeHHlO co CJIIe:lKHhIlolH.

neCTphIMH KOMIIneKCaMH HIDKHero p;eBOHa. Kp~e

3JIeKTpoconpOTHBJIeHlUl 'reTKO KOPpeJIMpYlOTC.II C reo-JJOrmeCKHMH npocPH.JISMH (lPm'. 3). ,lI;OKa3aHa

IIpn-rO~HOCTh MeToAa 9JIeKTpoconpoTHBJIeHHH p;ns aep;eHKH nOHCKOB K pa3Be~ 3anel'KeA HKlKHep;eBOHCKHX

KBaP-~TOBhIX IIeC"IaHHKOB.

nOnOlKHTe.JIhHhIe cPK3WIecIOle CBOtiCTBa lUOKHep;e-BOHCKHX neC"laHHKOB onpe~eJImoT HX npnrO,tllfOCTh B Ka'leCTBe CTponTenhHOrO MaTepnaJIa B KOMMYHaXL-HOM n HHlKeHepHoH CTpOHTeXLCTBe, a TaKlKe B Ka-'1eCTBe ~opo1KHOrO KaMHS H B npon3BOp;CTBe nony-cpa6pmtaTOB (Ta6JI. IlI).

Cytaty

Powiązane dokumenty

The current level of the inflation target (2.5%) protects the Polish economy against the zero lower bound to a signifficant degree.. However, its potential reduction would

gw – average monthly gross wages and salaries in enterprise sector, grand total, unep – registered unemployed persons in thousands; uner – registered unemployment rate in %; pem

Jarvik (1942) d istinguish es t he following branches of the N.maxillaris in Eusthenopteron: 1) the r amus i nfr.aorb italis, e nteringfhe n asal cavity t hro ugh the &#34; fen

Widespreading of thick synchronous ice-dam series at a distance of about 1000 km (from the North Sea through The Netherlands, the Lower Elbe and the Lower Oder to the

portance. have been ident'i!fiioo. Three forms, Polygrw.:thus ancyrogna- thoideus Zi.1egler, Schmidtognathus aff.. ACTA GEOLOGICA POLONICA, VOL.. PolYI1nathu8

In the investigated borehole sections of the LoWer Carboniferous of the Lublin Upland, · the lowest ca~OOnate beds comprise seVeral reef structures lacking at all

Owing to the continuous uplift of the western part of the East-European pIat- fQrm beginning with the Late Silurian, and especially amplified beginning with the

Dur ing the mid dle and up per Pridoli, how ever, a fa cies dif fer - en ti a tion starts in the Morava Unit with lam i nated clayey lime - stones (eosteinhornensis cono dont