Metodyka zestawiania mapy współczesnych ruchów skorupy ziemskiej

kich,

jak

trzc;:sienia ziemi (polozenie epicentr6w);

·

zmiany

stanu naprc;:zen obserwowane w postae!. stref

~:beIndJe~ IW

ikMTych

~j'f4 mf;l E07le<l!imy

t

sbrtelfy

spr~ 0 'WIi~ych ~ 1IlBiJt'~, zw~

jpO'1Jiomych,

lllir!

to

wymka z

~il In:&

podstawie cic;:zaru nadkladU; mlody wulkanizm itd.) .

.

5. Wynf.k6w badail geofizycznych w szczeg6lnoki

~W1imel1lryamYK!'h

d sejiSlmicmych,

kt60re

1IlP.

IllI&

db-~

Polski

dajl4

dla

t)'lCh

ce16w

nIlIJlepsze

wy·nikJ

IW ~e

s1lrulkJtiulnlllj

pi.~ ~2IIl~.

Plrzy

~~

wymden.iJonydh

wyzej

c~­

. kOw

rw

1NIfWIi4'zairrl'll

do

&1rwleEdoon"m

~.

ge-odezy)Illym.1

r.t,JJCIhhw

aI:rorn.1py

~j

ust1III1J1e

morima,

kItOry

r£'1DIich

IW

dan

·

ym

~

:tInIIkfmvae

i:I;rorina

ja.-SUMMARY

RemembeIrtiJnig

the

vmtIa'fians

of the

IIllOvEmelllJts

of

title

ElIIJl"I;h

ICIl'IWlIt

iJD

1tiimIe

amid

rflhed!o

llon.g-'IleIrm

1:eIJIdeIn-ci!e&

(W.

C. KowaIski, 11968)

one

bias

Ito

,t8ike

If.nto

8K:IOOUIlt.

by

~lQdalIg

dlaIritI!

.

of

the

r.eoent

:move-ments

o~

the earth crust on the base of the phecise

twkJItold

g.eodeBilc

BUIl"Ve.ve

(cansidert!nlg

daa

IIliC:aJ!lIIfiJ

of these surveys): the character and strike of

geo-logical structures in every known tectonic cover; the

d!hffereooes of

~

of

I8IedJmeDts

end

It!bteir

fa-·aiJeB ..,..

.~y

'in

neogesn'lc

8IIld

quaJr'tElmlaJry

geldi-men1a; Ibhe

I(lOI!IiIflIan. :of

the

.~ .4lI1~

BlIid

Ibhe

oelmJraiotler

aIIlId

:the

I1tntena'lJty

CJl

the

.geoldy-namdc

processes,

/Which

~

be

~

of

kIlO-'VIE!mE!Ilots

IOf

ttble

eIIl'Itih

crust;

mik:I

IaH.so

&$

aa!J.

IreSIUiIJbs

.

of

goophyslllc. ~lfJians ~y

'tihe

~­

metlrlc

and

saiaDiJe

anes.

·

Translated

by

the author.

PE

.

3IOME

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oc06eRHOCTH

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