o.
~a
p H Xl It Hi!:tt.
~.-
,l(Hltl!:'H't H3 ItOHKP~ -cem'apm!: yrom.Horo 6acceAHa KJIa~Ho. Acta U.niversitatls C&roUnae. Geologica.Ht
3, 1963. ·10. 3a
p H Xl It 51 a 11. B. - MHsepam.HbleHOBOofipa-30BaHKR B KOHXpe~ yrJIeHOCHhIX OTJIo:m:eHl!Gl BOCTO'IH&IX pmtOBOB .n;o:a6acca. Bec'l'RKK Xaph-ltOBClt. yH-Ta.
eepr.m
reorpaq,H'lecJ.taR, BhIIL · 2, 1964.11. 3 a p H Xl K Hall. B. - 0 reoxHMH"lecltOa no~ B~CTK MaJIhIX SJIe1l[eSTOB B ~areHe3e. .n;0ItJI. AH CCCP, '1'. 163, .Ni 3, 1965.
12. 3
a p
K D; It H·a 11. B. - OcdlSeBBOCTH XHMJI3M8 BhJ,D;e.nemdl: ~CYJIbq,H~a :m:eJIe3a pa3JIH'lHoro re-He3HCa B yrJIEmOCHhIX OTJIQ:m:eHKJIX; MHHepaJI'. eG. Jh.BOBClt. yH-Ta, .Ni 19, BhIIL 4, 1965.13 .. 3 a PH Xl It H a IT. B. - OcOl5esHoCTH :xmm:3Ka MHHepam.Hl>IX HoB006pa30BaHm,t B ltO~X -oCetI'l'apHIIX .n;oH6acca • .D;OltJI. AH CCCP, '1'. 167, .Ni 2, 1966.
14. KOHcTaBTHH.oB M. M. - 3lt3OreHHb1'e
cym.-q,~ cBKBD;a ·K D;KHKa. Bonp. MHHepaJIOl'KK
oca~o'mhlX 06pa3OBaHm!:, ltH. 2. H3~-BO JIbBoBCK'.
YHJ.l'a, 1954.
15. JI ~ 3 ape H It 0 E. ~ - 0 raJIeBH'l'e' K
xam.-Komsp~e B <l>ocq,OPHTOBldXXOBKp~
110-·~omm. MKHepaJIOr. c6. Jh.BOBClt. reoJIor. 06~.,
Ht
1. 1947.16. JI a 3 ape H It 0 E.
K. -
Cmmlta'l'hI K3 KBapD;eBo--ltap6oHa'l'BhlX :m:KJI Hal'Om>HOro ltplDKa.MH-BepaJI. c6:. JIhBO;BClt. reoJIor. 06m;. .NI! 4, 1950. 17. JI K H ~ r p eBB. - MHHepaJIbBhIe
MeCTopo:m:-~eHHJI. M-JI.,
1934-18. JIorBKHeHKo H: B. - 0 ri03~eM ~are
He3e (sIIKrEme3e) ~OHeqxHX ltap60HOBbIX DOPo.~. H3s. AH CCCP, cep. reon., M 7, 1957.
19. M a JI H HOB
C
It m!: ~. M. ~ M30r0IIBl>Ift 00CTaBcBHHD;a iK3 Cym.q,~OHOCHhIX <l>oc<PoPHTOB 110-~OJIHH.
feoxmom,
NR 2,. 1959.20. 03 e Po B a H. A. - IIepBH'lBhIeOpeOJIld pae-CeJIBH.f.[ PTYTH. Bonpochl reoXHMHH, IV, ·H3~-BO AH CCCP, M., 1962. .
21. CTapKKoB B. C., OJIbXOBCKHa· f. 11. - . KOHJq)eD;KoHHhIe 06pa30BaHHR K3 aaJIesCltKX
SUMMARY
Explanation of the ' genesis of the mineral for-mations that fill in the contraction fissures in sep-tarian nodules is not only of theoretical importance, but may also be useful in elucidation of numerous practical problems.· Such a circum,stance has forced the present author
to
begin once more the research on this problem and to continue the discussion with the Polish scientists.As· concerns secondary mineralization innodu-les, the rich specialistic literature does not explain such important problems as for example the age of mineral substance that fills in the contraction fIs-sures, the sources· of material, as well as the action of infilling. In his article the author does · not try
to
make any detailed literature review andto
ex-plain the problem definitively. Based on his own investigations of mineral formations in carbonate concretions found to occur in the coal-bearing de-posits cif the Donets Basin in the Soviet Union, andin the coal basins of Kladno and Ostrava in Cze-choslovakia, Lower and Upper Silesia in Poland, as well as in the basins of Scotland and Northern . England, the author' presents several conceptiorul that may contribute
to
the explanation. of the pro-blelDs here ·considered.6TnolKemdt
CesepHoA OCeTmi: :H JOt:iaaiteHHe.
Tp. CesepOltaBlt83Clt. ropsOKeT8JIJIypr. KB-Ta, BhIIi. 16, 1961.
22.
C '1' P a jc 0El H. M. -
.n;JtIlreues· OC~ltOB H eoo 3H8~eHHe ~JI.f.[ oc~oqsoro py~006pa30BasHH. Hs-BeCTHR AH CCCP, cep. reoJI., .Ni 5, 1953.23. C T P a x 0 B H. M • ..:... OcHOBbI TeoPHH JIHTOrearoa.
T. :0;. H3.D;-BO AH OCCP, 1969.
24.
~e
pc
11[a u
A.E. -
0
MHBepanoI'KH ltaMemmy-rom.BhIX OTJIO:m:eHHA: oJtpeC'l'BocTeiA r. BopoBJAK. . H3Bec'mfJI AK'a.D;ellHK HayK, cep. 6~ '1'. IX,Ht
1~,1915.
25. X a JI H
cil
a - 3 8 ~ e "i. M., A 6 6 a COB a C.M:
-~ePH'1'OBble 38JIe:m:K .n;arec'l'8Ba. H3A-IIO AH CCCP, . M., 1963.
126.
B
IOUII.' gu :ligno n iP. -IDi.dld!IIe
IdJu &ilurien et du houiller de Belgique,Ann, Soc. geol. Belg. Bull. 11911:11-1963 (19M).2'1. Gtr·uszclZyk H., Ku b'isz J. - 0 Il~
'WY-~h oddaoLtu
rw
~. KWl!d. geo!l., 4,Nll'l',
.1960 •.28. Ko n t a J. -Jilove minerily Ceskoslovenska. tNa'kl
CSA
V, lPInIIba, :uI67.~9. P 0 v 0 n d raP., S la n sky E. - Nove vtskuty dickitu v Ceskoslovensku. Acta Universitatis Caro-linae. Geologica, Nr I, 1964.
30. S k 0 l! e k V. - Karbomitove konkrecie v uhlono- .
ISIIlYcti. eeclimemlbecJh Osttre'ViSIklo-KalJ:rVd'DSke IPfImve. SIl.
Usltiiad.
IUBIt.eivI\l ~l. 0dId. ~. 28, 11S6d..CUI. S'Iloa'h 1L.,:Siilkora W. - .~ sbopnlia
1Jjp(Jrq~
iSItruJktIn.JIry
mlinelraiaw
~....
old!nd1nI. Spr8IW. 1£ lPQ!Iiedrz. kIoo:n:. ~
PAN
IW Kira-llrowIie, 1966.32. W 0 j c 1 e c how ski J., Z i 0 ID e k J. - 0 wyst~
powaniu sfalerytu w syderytach serif rtidnej
w
l..~czycy. Prz. geol. nr 7, 1966.33. Wojcdecbo'W's!k:i J. - ·W I!(mIIWlie
genezy
mi.-~,
rw
~~h.:nbIdem.
IIlIr l~ 11968.
3:4.
Za'lri!,olki IP. W. '- 0 ,g)BlleZfemin.erllliaw IW S'1JC7A!-linach kontrakcyjnych w~g1anowychkonkrecji-~. 1DbiIdml.
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