Badania tektoniczne a możliwości odkrycia nowych złóż surowców mineralnych na Dolnym Śląsku

(1)

(2)

SUMMARY

The best reconnalssance ot the

.

more important

.

irurfaceand deep tectonic structUI'es Is a basis

in

se-arch tor new

minerał

deposlts within the

tectoni-cally

.

complicated areas ot the Lower Silesia. Such

a

reconnaissance of the deep large structures, among

others

,

of granitoid and basic intrusions, may be

:IlaIaitilt.arbed

,by se!llli!-dataUed

ma~eIII«:

8IIld

~UnIe

.

1ric

&UJrveys.

.

'I!he

iilnVlEi9t~

ot

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tinIeiaIr

.

6JlId

a<reaJ

~

and

BpIaICIe

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1flime

1iJnteru:'Ieia-'liions

maY

be

heljp1!uł

'ID

:the

1l'IeJOOIlna.1ssa.nc.e

'Cd

,

1Ihe

.

main tecobonlic

Sbrudłulres,

as.

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waj"

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ibo

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~~

F1rom.

tbe

~

paInt

of

geo-metrd.cIlIl

tecto.h.iics

tbIe

tolfuwti!nlg

QepoQ\Its

may !be

d~SIbeId:

pos

.

t-deforma,1liooaIl

'

depdBits -

f.ormed

~ID łtIbe ~xist'in,g

teaboInic l!IbruIcflutres and

~;

sjlnd~ ~

-

furmed

alt :Ilhe

łlime

ol

lf41Ie

prodIuctiJOln,

ol

tec'boIndJe

lSIbru'C!l;,ures,

III~'

pre-def.dr-lnB.tiiona1

deposiJtB

'~

mt

Irelated !to

goometrka1.

:t.ec-tonics. After their formation they, naturally,

may

UlDdeIr,g<>

ltecItooliC

'

defurma1llnn.

To

othe t)'lPe&

men!jjjo..

ood

above

bellCC1lg deposi'ts

of

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ol

,

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prQdt<ieal vallue.

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