Iskalni niz je ali predolg ali pa vsebuje preveč besed.
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morska gladina
1 Objavljeno
pravo
Ur. l. RS, št. MP 2000-30
.9 Stanje morske gladine
.9 Sea state
2 Objavljeno
pravo
Ur. l. RS, št. MP 2000-30
da je snov na morski gladini olje; da količina izpuščenega olja ne pomeni kršitve konvencije; da olje izteka ali je izteklo z določene ladje ter o identiteti ladje.
that a material on the sea surface is oil; that the quantity of oil discharged does constitute a violation of the Convention; that the oil is being, or has been discharged from a particular ship; and the identity of the ship.
3 Končna redakcija
zdravje
DRUGO: TRANS
V zaporedju plasti se zrcali pozno paleocenska morska transgresija oz. dvig morske gladine.
In the succession the Late Paleocene transgression or the sea level change is reflected.
4 Končna redakcija
zdravje
DRUGO: TRANS
Ambientalno spremembo povezujemo z naglim evstatičnim padcem morske gladine v zgornjem turoniju (Haq et al., 1987).
The environmental change is associated with rapid eustatic drop of the sea level in the Early Turonian (Haq et al., 1987).
5 Končna redakcija
zdravje
DRUGO: TRANS
V poznem paleocenu je morska transgresija oziroma globalen dvig morske gladine prekril platformo južnozahodne Slovenije.
The Late Paleocene transgression, or the global sea level-rise, covered platform in SW Slovenia.
6 Končna redakcija
zdravje
DRUGO: TRANS
Zanimiv prispevek k poznavanju globalnih oscilacij morske gladine v zgornji kredi so podali Summesberger in sodelavci (1996a).
An interesting contribution to the knowledge of global oscillations of the sea level in the Upper Cretaceous was presented by Summesberger and others (1996a).
7 Končna redakcija
zdravje
DRUGO: TRANS
Padec nivoja morske gladine pod rob karbonatne platforme in njen ponovni dvig je povzročil nastanek nove sekvence na platformi.
The decline of the sea level below the margin of the carbonate platform, and its renewed rise resulted into the deposition of a new sequence on the platform.
8 Končna redakcija
zdravje
DRUGO: TRANS
V zgornjem turoniju je nagli padec evstatičnega nivoja morske gladine (Haq et al., 1987) prekinil nastajanje Repenske formacije.
In the Upper Turonian the sudden drop of the eustatic sea level (Haq et al., 1987) interrupted the deposition of the Repen Formation.
9 Končna redakcija
zdravje
DRUGO: TRANS
Danes še ni enotnega mnenja o tem, kako se je zgornjesantonijsko-campanijski evstatični dvig morske gladine odrazil na sedimentih Tržaško-komenske planote.
At present there is no unified opinion on the reflection of the Upper Santonian-Campanian eustatic sea level uplift in the sedimentary rocks of the Trieste-Komen plateau.
10 Končna redakcija
zdravje
DRUGO: TRANS
Dobro je definirana poznopaleocenska, thanetijska transgresija oz. dvig morske gladine, ki je po 5 milijonih let prekrila celotni prostor sedanje SW Slovenije (tab.1,3,4,5,7; sl.3,10).
On the top of this succession, well defined is the Late Paleocene Thanetian transgression resp. rise of the sea level that covered after 5 million years the entire region of present SW Slovenia (Pls.1,3,4,5,7; Figs.3,10).
11 Končna redakcija
zdravje
DRUGO: TRANS
Nastanek aptijsko-albijske emerzijske faze na kartiranem ozemlju povezujemo s splošno znanim padcem evstatičnega nivoja morske gladine na Dinarski karbonatni platformi (Haq et al., 1987).
The origin of the Aptian-Albian emersion phase on the mapped territory is associated with the generally known eustatic drop of the sea level on the Dinaric carbonate platform (Haq et al., 1987).
12 Končna redakcija
zdravje
DRUGO: TRANS
Kljub vsemu pa lahko o starosti spodnjega dela formacije sklepamo s pomočjo evstatičnega padca morske gladine v zgornjem turoniju (Haq et al., 1988), ki je povzročil nastanek onkolitnega horizonta.
Regardless of that, the age of the lower part of the formation could be roughly assessed by means of the eustatic drop of the sea level during the Upper Turonian (Haq et al., 1988) that resulted into the deposition of the oncolite horizon.
13 Končna redakcija
zdravje
DRUGO: TRANS
Nastanek plasti z amoniti se časovno ujema z rastjo morske gladine v zgornjem santoniju in campaniju, torej s časom druge pelagične epizode na Dinarski karbonatni platformi (Gušicy & Jelaska, 1990).
The deposition of the beds containing ammonites corresponds temporally to the uplift of the sea-level during the Upper Santonian and Campanian, that is during the time of the second pelagic episode on the Dinaric carbonate platform (Gušicy & Jelaska, 1990).
14 Končna redakcija
zdravje
DRUGO: TRANS
Ta sprememba nivoja morske gladine se je odrazila v hitrem litološkem prehodu iz kalcisferskih apnencev v plitvovodne biomikritne apnence, pogosto z izsušitvenimi porami in lokalno v onkoidne apnence.
This change in the sea level had its expression in a rapid lithologic transition from calcispheral limestones to shallow marine biomicritic limestones, often with disiccation pores, and locally to oncoidal limestones.
15 Končna redakcija
zdravje
DRUGO: TRANS
Podobno kot pri Komenskem apnencu tudi možnosti za nastanek Tomajskega apnenca ne moremo preprosto povezati z globalnimi dogodki oziroma oscilacijami morske gladine, ki naj bi vplivale na spremembe biotopov.
In the same way as with the Komen limestone also the possibilities of formation of the Tomaj limestone cannot be correlated simply with the global events, as oscillations of the sea level, that might have influenced the change of biotopes.
16 Končna redakcija
zdravje
DRUGO: TRANS
Najpomembnejši geološki dogodek na meji cenomanij-turonij je bil evstatični dvig morske gladine (Haq et al., 1987), ki je povzročil potopitev številnih platform in grebenov (Arthur & Schlanger, 1979; Jenkyns, 1985, 1991; Weimer, 1988; Hine, 1993).
The most important geologic event at the Cenomanian-Turonian boundary was an eustatic uplift of the sea level (Haq et al., 1987) that caused submersion of numerous platforms and reefs (Arthur & Schlanger, 1979; Jenkyns, 1985, 1991; Weimer, 1988; Hine, 1993).
17 Končna redakcija
zdravje
DRUGO: TRANS
Vendar Summesberger in sodelavci (1996a,b) menijo, da lahko tudi nekatere višje nivoje Tomajskega apnenca znotraj Lipiške formacije povežemo z oscilacijami morske gladine v sklopu santonijsko-campanijske transgresije na Dinarsko karbonatno platformo.
Yet Summesberger and others (1996a,b) believe that certain higher levels of the Tomaj limestone within the Lipica Formation could be associated with sea-level oscillations of the Santonian-Campanian transgression on the Dinaric carbonate platform.
18 Končna redakcija
zdravje
DRUGO: TRANS
Šribar (1995) in Šribar s sodelavci (1995) postavljajo med formacijo 3 (kar približno ustreza Sežanski formaciji) in formacijo 5 (kar približno ustreza Lipiški formaciji), formacijo 4, katero interpretirajo kot rezultat zgornjesantonijsko-campanijskega evstatičnega dviga morske gladine.
Šribar (1995) and Šribar and others (1995) placed between the Formation 3 (that corresponds approximately to the Sežana Formation) and Formation 5 (approximately the Lipica Formation) the Formation 4 which has been interpreted as the result of the Upper Santonian-Campanian eustatic uplift of the sea level.
19 Pravna redakcija
DRUGO
temperatura morske gladine
sea surface temperature
20 Pravna redakcija
DRUGO
SE SKLICUJEJO TUDI na določbe resolucije Generalne skupščine 44/206 z dne 22. decembra 1989 o možnih škodljivih učinkih dviganja morske gladine na otoke in obalna območja, zlasti nizko ležeča obalna območja, in ustrezne določbe resolucije Generalne skupščine 44/172 z dne 19. decembra 1989 o izvajanju Akcijskega načrta za boj proti širjenju puščav;
RECALLING ALSO the provisions of General Assembly resolution 44/206 of 22 December 1989 on the possible adverse effects of sea level rise on islands and coastal areas, particularly low-lying coastal areas and the pertinent provisions of General Assembly resolution 44/172 of 19 December 1989 on the implementation of the Plan of Action to Combat Desertification;
21 Pravna redakcija
DRUGO
Za namene točke 8A001.b "samostojno delovanje" pomeni popolnoma pod vodno gladino, brez cevi za zrak, delovanje vseh sistemov in križarjenje pri minimalni hitrosti, pri čemer lahko podvodno vozilo varno uravnava globino samo z uporabo globinskih načrtov, brez potrebe po podpori ladje ali podporne baze na vodni površini, morskem dnu ali na obal,i in z uporabo pogonskega sistema za podvodno ali površinsko uporabo.
For the purposes of 8A00l.b., 'operate autonomously' means fully submerged, without snorkel, all systems working and cruising at minimum speed at which the submersible can safely control its depth dynamically by using its depth planes only, with no need for a support vessel or support base on the surface, sea-bed or shore, and containing a propulsion system for submerged or surface use.
22 Prevajalska redakcija
izobraževanje
CELEX: 32002D0834
povezanost fenomenov (na primer nihanje Severnega Atlantika, El Nio in spremembe morske gladine in oceanskega kroženja);
associated phenomena (e.g. the North Atlantic oscillation, El Nino and changes in sea level and ocean circulation);
23 Prevajalska redakcija
izobraževanje
CELEX: 21998A0623(01)
Ravne temeljne črte se ne smejo potegniti na plitvine, ki so suhe ob nizkih vodah, in ne od njih, razen če so na njih svetilniki ali podobne naprave, ki so stalno nad morsko gladino, ali če je potegnitev temeljnih črt na take plitvine in od njih splošno mednarodno priznana.
Straight baselines shall not be drawn to and from low-tide elevations, unless lighthouses or similar installations which are permanently above sea level have been built on them or except in instances where the drawing of baselines to and from such elevations has received general international recognition.
24 Prevajalska redakcija
izobraževanje
CELEX: 21998A0623(01)
Te temeljne črte se ne smejo potegniti na plitvine, ki so suhe ob nizkih vodah, in ne od njih, razen če so na njih postavljeni svetilniki ali podobne naprave, ki so vedno nad morsko gladino, ali če je plitvina, ki je suha ob nizkih vodah, v celoti ali deloma oddaljena od najbližjega otoka največ za širino teritorialnega morja.
Such baselines shall not be drawn to and from low-tide elevations, unless lighthouses or similar installations which are permanently above sea level have been built on them or where a low-tide elevation is situated wholly or partly at a distance not exceeding the breadth of the territorial sea from the nearest island.
25 Prevajalska redakcija
izobraževanje
CELEX: 32003R1291
Morfološko in strukturno leži območje, kjer se proizvajajo žitarice, na apulijski planoti, ki se je izognila vdoru morja in je bila od mezozoika do današnjih dni nad morsko gladino, kar predstavlja posebnost, saj je to edini predel Apulije, kjer so se ohranile strukturne, geomorfološke in okoljske značilnosti, podobne prvotnim.
Morphologically and structurally, the cereal-growing area lies on the Apulian plateau, which escaped from being covered by the sea and has always been above sea level since the end of the Mesozoic era to the present day, a peculiarity of the area since it is the only part of Apulia with characteristics that are similar to the original structural, geomorphological and environmental features.
26 Prevajalska redakcija
izobraževanje
CELEX: 32003R0149
Za namene točke 8A001.b "samostojno delovanje" pomeni popolnoma pod vodno gladino, brez cevi za zrak, delovanje vseh sistemov in križarjenje pri minimalni hitrosti, pri čemer lahko podvodno vozilo varno uravnava globino samo z uporabo globinskih načrtov, brez potrebe po podpori ladje ali podporne baze na vodni površini, morskem dnu ali na obal,i in z uporabo pogonskega sistema za podvodno ali površinsko uporabo.
For the purposes of 8A001.b., 'operate autonomously' means fully submerged, without snorkel, all systems working and cruising at minimum speed at which the submersible can safely control its depth dynamically by using its depth planes only, with no need for a support vessel or support base on the surface, sea-bed or shore, and containing a propulsion system for submerged or surface use. 2.
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morska gladina