Zeitschrift für Angewandte Geologie: Band 24, Heft 2 Februar 1978 [Reprint 2021 ed.] 9783112562024, 9783112562017

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ISSN 0044 • 2259

ZEITSCHRIFT FÜR ANQEWANDTE QEOLOQIE

A U S DEM

INHALT

Pakow, B S. Zur Mmcrogcme von Gebieten autonomer Aktivierung, dargestellt am Beispiel des Done/.beckens F ö r s t e s , W., Hähne, R.; W a l d e , M.; Kühne, R. Zur Notwendigkeit komplexer geologischer Vorarbeiten für den Abbau von Tonlagerstätten T h i e k g ä r t n e r , H.

HFRAUSQEQFßFN

Substantielle Rohstoffklassifizierung und -ausblockung in Kalkvorkommen

VOM

ZENTRALEN QEOLOQISCHFN IM A U F T R A Q

INSTITUT

DES

Kaemmel, T.; M ü l l e r , E. P.; Krossner, L.; N e b e l , ,!.; Unger, H.; Ungethüm, H. Sind HgPb 2 und (Hg, Pb), gebildet aus natürlichen Begleitkomponenten der Erdgase der Lagerstätten der Altmark, Minerale?

M I N I S T E R I U M S F Ü R C/EOLOC/IE

S e i f e r t , A. Methodischer Beitrag zu He-, Ne-, ArIsotopenuntersuchung an Grundwäs-

A K A P E M

IE - V E

R L A Q

B E R L I N

HEFT

Ä

BAND 24 FEBRUAR 1978 SEITE 5 7 - 1 0 8 EVP2,— M 34114

INHALT

COitEPÎKAHME

CONTENTS

PANOW, B . S .

Zur Minerogenie von Gebieten autonomer Aktivierung, dargestellt am Beispiel des Donezbeckens

K MiineporenHH oöjiacTeii aBTOnoMiioñ aKTHBiiaaiíHH — noKasaiio n a npiuiepe ÍJoneiiKoro 6 a c c e i i n a

On the Miucrogcny of Areas of Autonomous A c t i v a t i o n — Illustrated by the Donetz Basin

57

FÖRSTER, W . ; HÄHNE, R . ; WALDE, M.; KÜHNE, R .

Zur Notwendigkeil; komplexer geologischer V o r a r b e i t e n für den A b b a u von Tonlagers t a u e n

K IieOÔXOaHMOCTIl KOMnJieKCHLIX reojioniMOCKHx npe;iBapHTejii>Hux paßoTax n a n paspaöoTiui rilHHHCTblX MCCTOpOH> iSM

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Zeitschrift für angewandte Geologie, Bd. 24 (1978), Helt 2 Panow / Minerogenie am Beispiel des Donezbeckens

65

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Peniaiomee P O B

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Macimaöii

MeTOjja

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HeMeTaM0p$H30BaHHHX

co-

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p o H B o r a o J K e i i H H X H HMewT p a m a w m e e TIMM

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Summary Problems of lithological-geochemical, chemical, isotopic and other investigations are discussed of the organic substance dispersed in rocks, as are those dealing with liquid and gaseous hydrocarbons. A decisive influence on the concentration and composition of fractions of the dispersed organic substance and on the degree of preservation is exerted by the stages of sedimentation and early diagenesis. The distribution of parentroclc suites of oil and gas in the sediments is determined by the lithogenetic stages considered, by which the formation, types and extent of hydrocarbons are decisively influenced. B y means of a modified method of regimen measures of processes of emigration are calculated in the upper 5 km of the non-metamorphosed sedimentary cover.

Literatur LARSKAJA, E . S . : Abmessungen u n d F o r m der Einschlüsse der dispersen organischen S u b s t a n z als F u n k t i o n der A u s g a n g s z u s a m m e n s e t z u n g u n d der Fossilisierungsverhältnisse. — T r . W N I G N I ; 1 7 5 , Moskau 1 9 7 5 . MAKSIMOW, S. P . ; BOTNEWA, T . A . u . a . : Ü b e r die Z y k l i z i t ä t der Prozesse der In: Mcshdunarodny geologitscheski kongress. Erdöl-Erdgas-Bildung. X X I V sessija. D o k l y d a sowetskich geologow. Gorjutschie iskopaemye. P r o b l e m y geologii i geochimii naftidow. I s d a t . N a u k a , M o s k w a 1 9 7 2 . MAKSIMOW, S. P . ; BOTNEWA, T . A. u . a . : K r i t e r i e n des genetischen Vergleiches zwischen E r d ö l e n u n d organischer S u b s t a n z . I n : Sb. Dostishenija organitscheskoi geochimii. — T r u d y C-go Meshdunarodnogo kongressa p o organitscheskoi geochimii, 3 4 9 — 3 5 8 , F r a n z i j a ( P a r i s ) , I s d a t . TECHNIP, Moskau 1 9 7 5 . W E B E R , W . W . : F a z i e s der Ablagerungen, die für die E r d ö l b i l d u n g günstig sind. - T r . W N I G N I , 5KflaioTe;i uecKHx,

BonpocM

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n

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Peniaiomee P O B

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MaTepHaJlbHO-öajiaHCOBoro

IOTCH

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Macimaöii

MeTOjja

OCaHOIHBIX n O K p O B H M X

no-

oßpaso-

({)imHpoBaHHoro

HeMeTaM0p$H30BaHHHX

co-

panHoana-

BJiHHHHe H a

H

H

KOH-

cxeneiib H

p o H B o r a o J K e i i H H X H HMewT p a m a w m e e TIMM

Kau

HA

MOBH-

BH'IHCJIH5

KM

nopoa.

Summary Problems of lithological-geochemical, chemical, isotopic and other investigations are discussed of the organic substance dispersed in rocks, as are those dealing with liquid and gaseous hydrocarbons. A decisive influence on the concentration and composition of fractions of the dispersed organic substance and on the degree of preservation is exerted by the stages of sedimentation and early diagenesis. The distribution of parentroclc suites of oil and gas in the sediments is determined by the lithogenetic stages considered, by which the formation, types and extent of hydrocarbons are decisively influenced. B y means of a modified method of regimen measures of processes of emigration are calculated in the upper 5 km of the non-metamorphosed sedimentary cover.

Literatur LARSKAJA, E . S . : Abmessungen u n d F o r m der Einschlüsse der dispersen organischen S u b s t a n z als F u n k t i o n der A u s g a n g s z u s a m m e n s e t z u n g u n d der Fossilisierungsverhältnisse. — T r . W N I G N I ; 1 7 5 , Moskau 1 9 7 5 . MAKSIMOW, S. P . ; BOTNEWA, T . A . u . a . : Ü b e r die Z y k l i z i t ä t der Prozesse der In: Mcshdunarodny geologitscheski kongress. Erdöl-Erdgas-Bildung. X X I V sessija. D o k l y d a sowetskich geologow. Gorjutschie iskopaemye. P r o b l e m y geologii i geochimii naftidow. I s d a t . N a u k a , M o s k w a 1 9 7 2 . MAKSIMOW, S. P . ; BOTNEWA, T . A. u . a . : K r i t e r i e n des genetischen Vergleiches zwischen E r d ö l e n u n d organischer S u b s t a n z . I n : Sb. Dostishenija organitscheskoi geochimii. — T r u d y C-go Meshdunarodnogo kongressa p o organitscheskoi geochimii, 3 4 9 — 3 5 8 , F r a n z i j a ( P a r i s ) , I s d a t . TECHNIP, Moskau 1 9 7 5 . W E B E R , W . W . : F a z i e s der Ablagerungen, die für die E r d ö l b i l d u n g günstig sind. - T r . W N I G N I , 5jiK>0pnT0BaH h noJiHMeTajijiHiecKan (fopMaiiHH. I l o j i y 'leHHbie H3 reoJiorHiecKHx, MHHepaJioreHHiecKHx H H30ToiiHbix HCCJICHOBaiiHñ AamiLie yKa3biBai0T n a n o J i i i r e n n o c H n o j u i r o m i o e BOCHHKHOBeime pyjiiioii MHnepaJiH3aiiHn.

IIpenrrojioraeTCH MaTeMaTHHecKH nojwepHíHBaHHLiíi MeTon BemecTBeHHOií KJiaCCHljHKaiIHH H BHÖJIOKHpOBKH CbipbH B npOHBJICHHHX Z3BeCTHHKa II npescTaBJiHCTCH n a oCHone m n o T e T H i é c n o r o npHMepa. n o pe3yjibTaTy ero npHMeHeHHfi pa3JiaraeTCH npOHBjieHne H3BecTHHKa Ha 6JTOKH onpenejieHiioro BeinecTBeHHoro CBOiicTBa H p a 3 J i H ™ o ñ reoMeTpHH. r p a i n m b i ÖJIOKOB onpefleJiHioTCH n o BCEM BKjnoieHHbiM B nccJieAOBaHHe napaMeTpaM. MeTon noJiynaeT aiítfieKTHBHOCTb npeHMymecTBenno TaM, r n e Hy>KHO OÄHOB peMeHHO yHHTbiBaTb iieKOTOpbie HJIH MHorne riapaMCTpLi ii rué aiiajiH3 OTiiomeHHii cuíiabiuaiiMíi noita3biBaJi cymecTBOBaHHe MHoroKOMnoneHTnoñ CHCTeMbi c He3aBHCHMbiMH KOMnonenTaMH. MeTOji IipHMeHHeMblä KpOMe HJIH npOfIBJieHHii H3BeCTHHI(a SJIH KJiaCCHlJlHKaUHH H BbiöjiOKnpoBOK B jiioöbix nopoAax Ha OCHOBC juoöbTx napaMeTpoB.

OEPCTEP, B . ;

X 3 H E , P . II n p .

K i i e o S x o A i i M o c T u KOMnxeKCHbix r c o n o r m e c K i i x i i p e A B a p i i T o i n . IILIX p a C o r a x n i u ¡ p a a p a S o T K H I JIMUHCTLIX M c c i o p o j K ^ e H H i i Z. angew. Geol., B e p j i n n , 24 (1978) 2, CTp. 67 — 74, 7 HJIJI., 1 TaOji., 5 JIHT. PaapaOoTKa MecTopowfleHHií PHXJILIX n o p o s MOweT UPHBGCTH n p n HesocTaTOHHbix HaénioAeHHHx rHflporeoJiorHiecKnx H noiBeHHOMexaHH^ecKHX OTHOineHiiH K pa3H006pa3HbiM GCJTOHíHennHM. H e nonycTHMi,te noTepn pa3pa60TKH HJIH 0TKa3 HMeioiiiHx cbipbeBbix s a n a c o B naCTO HBJIHIOTCH HenocpeflCTBeiiHoa nocJienoBTeJibHOCTbK). H a npmuepe rjiHiinCToro MecTopoíKAeHHH noKasLiBafOTCH BHJI H oSiieM rHnporeojiorHHecKOii H n0HBenH0MexaiiH4ecK0ii paanezuin Kan H KOMnjieKCHan oCpaGoTna u c e x HMeiomHxcn reonorHnecKHx, RHHPOREOJIORHÍECKHX H n o i B e m i o MexaiiHHecKHx nanHbix H napaMeTpoB. 3TH HCCJieaOBaiíHíi n03B0JiHi0T y>ne B paHHoii CTaHHH nonroTOBitH pa3pa6oTHii BHBOHI.I OC o;itHflaeMbix ropuo-TexHHHecKiix npoOJieniax., XDIIE, P . ; PAUIEP,

K.

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Z. angew. Geol., EepjiHH, 24 (1978) 2 CTp., 7 4 - 7 8 , 3 HJIJI., 4 TaBJi., 17 JIHT. K a K BKJiaa h j i h peKOHCTpyKiiHH reHe3Hca ocTaTOiHwx b o a H KaK n p o s o j i íiieime npeíKiibix p a 6 0 T nepejiaioTCH c n e p B a onbiTbi npH HoGbiie TaKHX n o » H3 Majio npoiiHiiaeMLix KaüH030iiCKHX nopoH. OnpeneJieHHe xnMB3Ma OCTaTOHHblX BOfl npH nOMOlHH MeTOfla OBJiaJKHeHHH n o KpiOKOBy H flp. iipHTHHecKH npOBepfleTCH. lllHpoKoe npocTpaHCTBO npHHHMaeT c n e p B a •rexHHHecKa TOJibHO TpyHHO peajrasnpyeMbie HccjienoBaHHH n o pa3MemeHnio H30T0Ü0B H n o coflepiKaHHio OJiaroponiibix r a 3 0 B B T a n n x B o n a x . IlepBbie aHaJiiiau 6'"O n BbiHCHeHHbiii (J)H3HHecKHii B03paCT no MeTOAy l l e - A r yKa3í,maioT n a BTopnqHoe aTMocíJiepuoe iijinrmne nepBOiiaHaJibuo MOPCKHX OCTaTOIHI.IX BO« PyneJIbCKOH rjIHIIbl. BOJIKOJIAKOB, HKOBJIEBA, B .

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Z. angew. Geol., BepjiHH, 24 (1978) 2, CTp. 9 0 - 9 6 , 4 HJIJI., 5 TaOJi., 37 JIHT. H a r a 3 0 B b i x MecTopoH