Iskalni niz je ali predolg ali pa vsebuje preveč besed.
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krovnina
1 Končna redakcija
zdravje
DRUGO: TRANS
V podlagi se nahajajao plasti vrhnjega dela maastrichtija, v krovnini pa apnenci thanetijske in ilerdijske starosti.
These Paleocene sediments overlie Upper Maastrichtian deposits, and are overlain by limestones of Thanetian and Ilerdian age.
2 Končna redakcija
zdravje
DRUGO: TRANS
Za tipični profil Lipiške formacije je bil izbran zgornji del profila Kopriva - Dutovlje, ki obsega njen celotni razvoj od Sežanske formacije v talnini do emerzijske meje z Liburnijsko formacijo v krovnini (sl.
For the typical profile of the Lipica Formation the upper part of the profile Kopriva - Dutovlje was chosen that comprises its entire development from the Sežana Formation below to the emersion boundary with the overlying Liburnian Formation (Fig.
3 Končna redakcija
zdravje
DRUGO: TRANS
Za tipični profil Lipiške formacije je bil izbran zgornji del profila Kopriva - Dutovlje, ki obsega njen celotni razvoj od Sežanske formacije v talnini do emerzijske meje z Liburnijsko formacijo v krovnini (sl. 5).
For the typical profile of the Lipica Formation the upper part of the profile Kopriva - Dutovlje was chosen that comprises its entire development from the Sežana Formation below to the emersion boundary with the overlying Liburnian Formation (Fig. 5).
4 Končna redakcija
zdravje
DRUGO: TRANS
V večini opuščenih odkopov apnenca blizu meje Sežanske formacije so ponavadi (zaradi blagega vpada plasti) odkopavali ekonomsko zanimive plasti Repenske formacije v talnini ali apnenec Lipiške formacije v krovnini.
In most of the abandoned limestone quarries that are situated close to the boundary with the Sežana Formation usually (owing to the gentle dipping of beds) the economically important beds either of the Repen Formation in the foot wall, or of the Lipica Formation in the hanging wall were quarried.
5 Končna redakcija
zdravje
DRUGO: TRANS
V najstarejših delih Lipiške formacije, torej v krovnini Sežanske formacije, se pojavlja foraminifera vrste Pseudorhapydionina mediterranea (De Castro), ki se pojavlja v zgornjem delu santonija in v campaniju na otoku Braču (Gušicy & Jelaska, 1990).
In the oldest parts of the Lipica Formation, which is directly overlying the Sežana Formation, appears Pseudohapydionina mediterranea (De Castro) that was found in the upper part of Santonian and in Campanian of the island of Brač (Gušicy & Jelaska, 1990).
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krovnina