6. K u h 1 J. - Surowce mineralne, 'bowarzYSZqce
zrozom
w~gla i d~h wykorzysltanie. P.rz. geol. 19'37,m
6. : .7.
iK
u h!l. J. - Kristall.otonsteine, die :in.Kohlenfl5.-zen
al& vuLkani&cheElemente .zu .bebrachten s.ind,
als leitftihrende IWrizonte !bei .der P.aralleilstel-l-ung
der
Floze dm oberscltlesischen lKioih[EmIbecke«l..
~r.
.
Fors.ch. 111960, C., H. 80. . ..8.
Kuhl
·
J.
,
K
'
ruszewS'ika
K. - f.upk!l ogniQ-' trwaleXikiwCe
ikTystall.cmre) 'Z. waxstw hW.skich w SlllsktHKr.8.kowskiln Zagl~i'U W~owYm jako horyrority przewodlllie' przy ,paralelizac,ij. polda-d6w ~~" ·.A!cta geoi. pol. 1965, vol. ~V, !!1I' 1.$.UMMARY
The aDticle shows that im. the Mi!ldW'ice mme the
. bentonite !Seam buillt up of'vo}canie ashes is covered Wl"lth psammiIMc tu~tes (:pyroclastic saniCl6ilones) - and crystall!lilne clayston~ (coal tonstein). The bentanites consistiaJ:g of fllite· and . montmorillonite, the rpredo- .
'
..
min8fl1'Ce
.of wbleh changes . along,· thestrike, are
thoughtby
the pregen't authorsto
bea
praduc't ofsedi'menta'f:ion' in a .
depper
water ba's'ln, where pH must have bee'.nofh~gh va'lue. The psammltic tuf-fitefS were sedimented in a more acid: environment, thus the volcanlc gla'Ss altered mainly tn'to. kaoldnlte, partly also into mon1morillonJte. and muscovite. On.the other
haA<Q.;
the cOal!. tonstein. bed that occurs in the seam 610 has been formed. under acilc1-humid condft'ion'S, . as proved by the pr~inooce of kao-ifinfte.9.
MIc
h a: J: elk: Z. - I1y l'OOnfrooryllandJtawe !Z: Ra-dzion'kowa na G6rnym Slq6ku. Zesz. rna'Wk. .A;GH, rozp. 319, 1005.10. iRosler
a
J., iPii.lchern W. - Die KoOblen-tonst.em.e 'aus den Steirnikohlenbedken van Zwikau-..:oe:t:mitz, Freital-Dohien (!bei Dreeden)un'!i
Do-lberlug. F:reilb. ·ForsC'h. ,l!Q67. C. ,2lil.L1.
lBiyezka
J. - ·KxytStlrlochemi.cme i Jf.i.zy.cznewla-emWDACi
mon1morylOlnitOw poziomu' ·bentoniwm:!-go ,w ikaribonie produktywrnym ZagI~G6mo-~eg(). 1Prz. gaol. 1967, m 10. . .
1.'2. S'21teilak J. - MOMiwoO&ci wytkorzystania
ben-too.dIt6w,
wystlWujllCy.ob
w
utrworaeh produktyw-nego klUibon·u. G. Z. W. Ibldem !l963, nor 5.PE3IOME
B CTaTbe ,D,OKa3bmaeTCR, '1ro B waXTe MHJIOB~e
Ha 6elftOBKTOBOM ImaCTe, 06pa3oBooweM:CJl Jif3 ~y11.
KaHH'Iec.s:oro neIma, 3a11.eraIOT nCaMlllHTOBbIe Ty(j;l-(j;lHTbI (II'H'POKJIaCTH"IeCKHe nec'lamtl!:H) H B:pHCTaJIJIH-'1ecKHR aprHJIJIHT (yrom.~ TOHWTeAH). BeHTOHHTbI, CJIOlKeBHbIe HJIJD.r:'l'O:M H MOHTMOPHJI11.0lDf'l'OM C
IIPe-06JI~aroIqHM KOJlH'lecri!OM TO o~oro, TO ,ltPyroro KOMDOHeHTa no IIPOCmpaHHlO, pacCMaorpHBalOTCH 00-TOPaMH KaX r.ny6oKo BO,qm.W: oca,qOK, 06pa30BaHHbIA B yCJIOBnJlX· BbICOKOro pH. TIcaMMHTO'Bl>Ie. TY(j;lqmTbI HaKOnJIJlJIHCb B 60JIee KHCJIO~ cpe,qe H D09TOMY BY11.-KaHH'IecKoe CTeKJIO B 9THX Oca,l{ltax npe06palKeao B KaOJlHHHT H B MeHbIIi:eft CTeIIeBH B MOBTMOPHJIJIOBHT H MYCKOBHT. Cnoa yrOJIhHOrO TOBIIITethia 06pa30BaJICJl B KHCJIOa - ~oa cpe,qe, '!TO BbIplUKeao npeo6lI.a-,qaRHeM KaOJIHHHTa.