Statystyczne pomiary rozkładu granulometrycznego jako wskaźniki odwzorowania dynamiki sedymentacji wodnej w czwartorzędzie

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SUMMARY

A modd of

geo:ogica:l struC'wlte 'wai;

made

with

the use of trEnd It'Jrfa.ce maps and disC'l'irninant fun-ction. Arualysis of that n::ociel made :.t iPO'Ssible

to

8:s'Sume existence of five envirOllllnents 0If 6~diment atioo Qf nanr-cohEs.ive soils in the Sl'ea studied. This subdivision

into

five sedimentaJry envk<:aunents was SU1bsequenUy verified with the cse of

IPtatistica1

tech-niques ialvolving correlatdoo

and

regression analysis of sta1tistical in.d:Jces of di£lbrlbu1ioo of !'l'IaJCti,OIllB. On that basis there were distinguiShed envtromnen'llaUy-09E!nsitive statdstiJeal paxameters (in 'that schem~ of analysis) which made possible preliminary approxi-ma'tion of the dynamics of sedimentaltion of the en-vironments analy~. Moreovilr, a hypoth:sis Wll'S put fOil"Ward that it is pcssdble rouse IStrutistioea:l-mat-hemCbtic analysis in lithological-facies identill"a1;ion (Jf non-ClOheaive soils. HOWever, it is a workiing hy

-pothes!s requliring furtheT mult:/ple teS'ts.

l"E3IOME

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