Z badań geologicznych w 1957 r. w obrębie antyklinorium kujawsko-pomorskiego

Jadwiga Dembowska

Abstract


GEOLOGICAL INVESTIGATIONS, CARRIED OUT IN 1957 WITHIN THE KUJAWY - POMORZE ANTICLINORIUM (CENTRAL POLAND)

On the background of the Kujawy - Pomorze anticlinorium there may be distinguished two second grade structures: the Zalesie (near Barcin) structure, and the Szubin structure.

T h e Z a l e s i e  s t r uc t u r e, indicated by a negative gravimetric anomaly, is situated in the depressed part of the anticlinorium, where its axial part is built of Malm sediments.

According to the interpretation of the seismic data, supplemented by result of drillings, we most probably are facing here a dome type. salt structure. On both  section (Fig. 2) and map (Fig. 1), the author presents a probable Zalesie structure. It appears from the geological interpretation of the seismic profile that the culmination of this structure lies between bore-hole Zalesie, situated on its southwestern and bore hole Złotowo, situated on its northeastern limb.


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