Górnomioceńskie osady ilaste Sudetów

(1)

(2)

(3)

(4)

(5)

(6)

2~'

¥

a

"nl"(ri

a

r

'

i . ...:

Wzoreowy

!Pl'ofil

s:Porowo-pyi-. " k<lwy' z g6tilamiocei:lBkiego , w~a bruDatnego

, z Pohiti· 'SrodIrowEi,j (zloZe Rogoflno). Ibidem Ilt1'

l58, 1961.: ' '

24; M 11 e

w

i c z J." ,G roe h 0 Is ik: i A. -

Trzecio-r~ mi~zy BoleslawcEml. i W:~lincem. Ibidem m: -15>1, 1960.

25. O!b e r c' J., D y j o;r S. - Mlodotrzeciorz~owe

ruchy tektoniczne w Sudetach. Prz. geol. 1968,

.nr

1'1.

26. '0 b El It' If:

J.,

:p

.y

'

J

<> r

S. -

Usokok sudecki

b~eZ-n,y {w drulw). " , , ' ,

27.

0 IS Z !I,:s

t

J. -

AnaUza pylkoowa ilow

torton-skich

ze

stwrych Gllwlc. Mon. Bot.

rt.

9,

z.

I, 1960.

28. R.u d Q 1 ph K. -:- Mikro.flottstische Unter~uchun.,. gen lterrtiiirer AIblagerungen Un nordlid:ien

Bog-'

men ..

Beib.

z.

'

Bot

.

Centrailbl. B~ 54. , ' ,

29. So b, 0 I El ws k

a

L. - RosliniloSl: plejstocenska z Syrnik on&d 'Wieprteni. Z booati czwa.Ilto.r~du

VI PcilsCe.Biril. iliG, nr 100, 11956. , 30. S

1:

u chi d k L. -PoUen analys,js :of the

mioce-, "

ne

'

depooits at Rypin. Acta' ,paleOoot. vol. 5, nr 2,

' 1964. " , "

'SU,MMARY

The results of the

!1'1eCenIt

geological ISOO

paloaeobo-t~ Ilt'llidlies ~

that

:pari of the Sudet!ic clay deposits,thought ISO :faT to,

represent

Quaternary dce-ltDa/1'~ lake clays, is, Considerably, older" and

can

,be ir~ 00 itbe U;pper

Miooene. These

~it

rest

in the

nor.th'enl

pari of !the Sudebes, wj.tbin

a leverung

plane,

mOaiftied

later by

young

tectonic

movements. '

It has

been' ~

on PaiaeOntologtical

ami-lySes' that 'the

.Vpper

~ clay depcmtos of the

Sudetes facialily

wiTesiPond

to

rthe lawer memberlS

of rthf! Poman serieS m <the Fare:.sudeM.e

bolOOk.

They were fur.med with'ion !the ;i.ntermountain ,basill1s =invaded, at the time of the (Poznan series, by the sea that

dn thIIs perdod existed ,in the area d! the Fare-Sudetic

block 'Thm .is 'also p-oved 'by the mdaroarganism

"Hystrix" foI.md

:to

OCC\U'

art

rthe

sites

here OOIlBidered. The :fJor:is.bic ~ lBSCertadned in itbe clay

deposits of the Sudetlic area, ~oned on the basis

of spme-a.ndiPOllen analysis,

is,

art

all

the

site

'inve&ti-gated,

highly approximate and, rtWical of rthe Younga-Tertiary period. ','

31.

S

z c z

e

pan

it

1

ti,w

i

c

z

s. -

Rozw6J

dollriyg6r-Ilego Bobru u kra~ a.~dododu wSudelach.

CZQS1:lp. geogr.

t.

23/24, 1954. ' . 32. T e ills e y r e H. - Tneci~d

w

Sudetach i Da

ich iP6lnocno-zachodnl:m przedpolu. Regionalna geologia PoISki; praca ~orowa,

t.

3, Krak6w,

1900. .

33. W a IJ. c

z

a kW. - , Sudety Klodzkie i ich IPl"zed-pole. Przewodnilk wycieczkowy ,IX ogolnq:101Bkie-go Zja2'Jdu Pal. TOW. GecJIil'. W'1'ocl:a'W, 1966 •

34. W ale z

a

k W. - Sudety. 'PWN W~.szawa, (1968.

35. 'Z i e m III ins ok a M. - 0 moZli'W~i paraieliza-cji poklad6w w~a brunatnego na podstlil",-,:ie

wy-nik6w ,analizy sporoWlO..p~wej.

Kwa1'lt.

ge~, 1964,

t.

8, (1;. 2. ,

36. Ziem·binska M., Niklewski J. - Stra-tygrafi.a i ~aleliZacja poklad?W wE:~a bJ::unatne-;go zloza Scinawa' na podstaWle analizy spt>rowo~

"-IPyfk:owej. 'Biul. ~G, nr 200. Z badan z.l6tWE:gli brunatnych'W Polosee. Tom I. ,Warszawa. 1.967.

37. T Eli c hID ii ill eT R. Die' ni:edert-heini:sche Bra<iinkohlelllfOrmation. Stand der Untemuchungen oUnd oMime Fragen. FOr'tschr. geol. Rheinl. u.

Westf,' J95B.

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