Uwagi na temat niejednorodności wgłębnej budowy geologicznej w NE części granitowej intruzji Strzegomia

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SUMMARY

The 1W0II"ks peddrmed aTe lWed, the :results of geqphy.siCBil ~es made i'l1 the

area

of ,the

strze-gam graDlit'e

are

<I!iscuissed.

ood

the che.m~ !Of the deep COIlJI;aot of the dn'tn,l'sdoo with flle adjacent l."IOICks is preeen:bed. 'Both t'he ZIOlle of negative iI"tlS!lSUvity anom'8l1lies and that of pailiif:ive lll180gDetlc aIlOlIlailies,

recorded

along

the

north-eastern margin

of the

!i'l1-tn.ulIiJoo,

are

broadly d:iseussed, and ItherJdo geological intet;pre1;ailll.oo lis

3iven.

A :possilbillLty of If;he

occum-en-.cen

of mmerd meta~Uc depoSits related to the granite II.s stressed; and a onecElss.tty !Is ElDlPhasized ooncerllllin'g

the

complex e1Bbamtion of the tresul'ts

abtained

du-ring the g.eqphyaloal su·rveys aJtIId .geological WIClIrks, with iUle P1lqlOSIe of

e1aIboraJting

the ooooeptioo of

f.l.'IIt.tber prospectiioos.

PE310ME

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