Univerzalno krigiranje do sada nije korišteno pri kartiranju geoloških podataka u Hrvatskoj. Međutim, radi se o jednoj od češćih metoda krigiranja, vjerojatno najprimjerenijoj u slučajevima kada su ulazni podatci obilježeni zajedničkim trendom. Upravo takvo obilježje vrlo je često svojstvo dubinskih geoloških podataka, a time i strukturnih karata. Kartirane plohe u nizu primjera imaju strukturni nagib prema jednoj strani svijeta. Često je niz geoloških struktura, poput antiklinorija, dio strukturne jedinice većega reda poput regionalne monokline. U radu je dan primjer prepoznavanja zemljopisnoga trenda u pružanju plohe EK markera Z’ u polju Šandrovac te uspješnoga kartiranja te plohe, odnosno dubinske varijable, univerzalnim krigiranjem.
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