Zagadnienie stopnia w grawimetrii

(1)

(2)

(3)

(4)

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I / " , /"

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/ " , ", Rye.5.

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Fig;-

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5:

-'''100a..._ LITEl\ATURA

1. 'J u.n g K. - Schwerkraftverfahren in der ange-wandten Geophysik. Leipzig .. 1961.

2. J u n k 0 w A. A., A fan a s j e w N. l..., Fie d

o-r ow a N.

A. ...:....

Intie1'lPrieltacija anomaiji Ag nad

:kontaktami i sbrosami, - Googieoltiech1zdat.

Mos-kwa

1001.-3. K () Z era ·A .. - . ZagadIllienie niekt6rych prawidlo-'

-wosci wyrst~uj~cych w ilosciawej inteI.'lPrErtacji

ani>m!l1ii sUy d~Zk*L Piraca doklt9l\9ka 1965, Bi-blioteka. AGH. K~aw.

4. M 1·11 s_ F. C .. ~ statistical methods. London 1955.

PE310ME ...

B rrpHpo,l(e BCTpeqaIOTcH HHOr,l(a TaKHe

reoJIOl'JI-qeCK~te. QlOPMbI, KOTopble C '!1paBHMe'l'pH'iecKOO 'I'O'Ilm 3pa!lMH . M~O a~'l.'b c nOO&OII(bIO

CTy'-neHl'f. K H!1M OTHOCHTCH c6POCbI, ropcTbI, !1pa6eHbI, fsoO . YCTYnbI. KOr,l(2 X£.p8KTeP aHOMimHH H cpopMa ui:pnBO~

~ OIIPaB,l(blBaIOT TaKoe 8InP0Kcm!HpOBaHHe, TO OB Ta-lWM CJIyq8e Ha oCHOBaBHH a'HOMaJIHH A.g l\IOCIKHO no-JIy<rnTb nOJIHYIO xapaKrepHCTJmY .8HOMaJIbHOI'O TeJIa.

SUMMARY

In the natuTe we often meet geological forms that,

from the gravimetricall. point of v.iew, can be

estima-ted a;p,prox.imately 8iS iSiaps.

Here, such fOTms belong as fauJ;ts, erosional

troughs, h~ts.

a,nil'

bi1:odms.

If both the cha'l'actJe:r of anomaly and .the shape of curve Ag suootantiate such an a~imaof;iO'Il then we can obtain, by meam of anomaly Ag, a complete information as

to

the disturbing body.

FOT this jpu'l'IPooe the au thar uses in!fier.re<latdic)Ds

ex1Lst:ing between the magndtudes Xextr.Wzz and