A G R E E M E N T

C O N V E N T I O N

Consequently, protein synthesis, t.e. factor VIII and factor IX is disturbed.

These procedures only deal with the frequency bands in which DVB-T is envisaged, i.e. 174 to 230 MHz and 470 to 862 MHz.

If the laboratory has reported the presence of a T/E ratio greater than four (4) to one (1) in the urine, further investigation is obligatory in order to determine whether the ratio is due to a physiological or pathological condition, except if the laboratory reports an Adverse Analytical Finding based on any reliable analytical method, showing that the Prohibited Substance is of exogenous origin.

If the administration consulted is responsible for a DVB-T station or SFN, the method of assessing compatibility given in Annex 4, Section E shall be used.

No consultation in the case of a converted analogue station into a single DVB-T station is required provided the e.r.p. is no more than the analogue e.r.p. minus 18 dB, and other technical characteristics are not changed or would reduce the probability of harmful interference.

(c) the proposed modification relates to the conversion of an analogue station into a single DVB-T station, provided the e.r.p. is no more than the analogue e.r.p. minus 18 dB, and other technical characteristics are not changed or would reduce the probability of harmful interference

The Republic of Slovenia shall ensure that the rate recorded for conversion between euro and national currency is that for the Republic of Slovenia published by the European Central Bank on the Internet at 14.15 C.E.T.:

This is consistent both with case law of the Court of Justice (Cf. notably case law on the "precautionary principle" in Article 174 (2) TEC (replaced by Article III-233 of the Constitution): judgment of the CFI of 11 September 2002, T-13/99, Pfizer vs. Council, with numerous references to earlier case law; and a series of judgments on Article 33 (ex-39) on the principles of agricultural law, e.g. judgment of the Court of Justice C-265/85, Van den Berg, 1987 ECR 1155:

In the literature such type of sedimentation is termed as palustrine environment or palustrine limestone (F r e y t e t, 1964; F r e y t e t & P l a z i a t, 1982). The authors studied Upper Cretaceous and Paleocene beds in southern France.

Mr T. E. Westerterp, State Secretary, Ministry of Foreign Affairs;

In the subdivision of Paleogene in Shallow Benthic Zones SBZ 1 - SBZ 20 the propositions of International subcommission for chronostratigraphic units of Paleogene stratigraphy are considered (J e n k i n s & L u t e r b a c h e r, 1992; O d i n & L u t e r b a c h e r, 1992).

In the Soča Karst area, T e n t o r et al. (1994) subdivided the whole succession into the Liburnia group (Gruppo Liburnico) and miliolidal limestone (Calcari a miliolidi).

The letters E, O, F, F+, T, T+, C, Xn, Xi and N do not form part of the symbol.

Foraminiferal associations from Thanetian beds (SBZ 3, SBZ 4) might be correlated, too (D r o b n e et al. 1988; P u g l i e s e et al. 1995; B r a z z a t t i et al. 1996; T u r n š e k & D r o b n e, 1998, fig.3).

Particularly interesting are the beds at the K/T boundary for their shallow water carbonate development and biostratigraphy, paleontology, sedimentology of Paleocene beds: (D r o b n e et al.,1988, 1989, 1994, 1995, 1996; P u g l i e s e et al., 1995; J u r k o v š e k et al.,1996a,b, 1997; D e l v a l l e & B u s e r, 1990; D e C a s t r o et al., 1994; C a f f a u et al., 1995; K n e z, 1994, 1996; K n e z & P a v l o v e c, 1990; Dasycladaceans: B a r a t t o l o, 1998; Corals: T u r n š e k & D r o b n e, 1998; abiota: D o l e n e c et al., 1995; O g o r e l e c et al.,1995; H a n s e n et al.,1995, 1996; M a r t o n et al; 1995; P a l i n k a š et al., 1996; O t o n i č a r & K o š i r, 1998; Late Cretaceous dinosaurs, crocodiles: D e b e l j a k et. al., 1999).

They were described in detail by G. S t a c h e in the years 1859 to 1920.

Geographically closest to NW part of our platform are Paleogene and Neogene sediments of Maiella region (P i g n a t t i, 1994; V e c s e i et al., 1996; V e c s e i & M o u s s a v i a n, 1997).

But, Stache's genera Lagynophora and Kosmogyra are still valid (B i g n o t, 1972; E r c e g o v a c, 1981; K n e z, 1996).

In the north part of Pyrenees occurs foraminifera Bangiana hanseni in profile La Cassino (C a v a g n e t t o & T a m b a r e a u, 1998, 239) in Danian beds and in similar depositional conditions as in the Čebulovica profile.

Classic ground for such studies are also nowadays next to Algeria (M e b r o u k & F e i s t, 1999) the Pyrenees.

Light composite wood-based beams and columns (including T-beams, i.e. beam/slab combinations):

We can correlate the restricted shelf environment (with periodical dasycladals) of the Čebulovica section with open shelf environments (with dasycladaceans) recognised in the Dolenja vas section (P l e n i č a r et al., 1992; B a r a t t o l o, 1998; T u r n š e k & D r o b n e, 1998).

Gastropods Stomatopsis Stache, Cosinia Stache and Kallomastoma Stache (S t a c h e, 1889, Pls. 1 - 6; K n e z, 1996) occur, too.

Their advantages were the following: large tests, complex inner structures, dimorphism, reproductive Čcles in accordance with seasonal food enrichments, " readiness " for speciations, increased diversity over a short period, seen through phylogenetic flourishment of few genera with many species (H o t t i n g e r & D r o b n e, 1988; H o t t i n g e r, 1997).

Similarity in fossil associations could be explained by existence of gyre (current stream) pattern in Maastrichtian and Paleocene (H o t t i n g e r, 1990, paleobiogeographic map).

Also here algae Lagynophora in Danian beds are predominant, and dasycladaceans along with foraminifera in younger beds (S l i š k o v i † et al., 1978; D r o b n e et al., 2000; T r u t i n et al., 2000).

The stable isotope analysis on?13C and ?18O indicate water temperature in environments where sedimentation took place, up to 27o and 30oC. The same values today have subtropic seas, like water in the gulf of Aqaba (R e i s s & H o t t i n g e r, 1984).

In relation to the section Dolenja vas, 5 km north of Čebulovica, the marine development prevails from K/T boundary till Thanetian beds, what indicates the closer position to the open sea in the northern direction (D r o b n e et al,. 1988, 1989, 1996; T u r n š e k & D r o b n e, 1998, fig.3).

Applying new methods, we confirmed the hypothesis by G. S t a c h e and M. H a m r l a about Paleocene occurrences of Lagynophora genus.

SW along the main road towards Divača, 2.5 km away from Čebulovica section, characean-bearing deposits, once described by S t a c h e (1880, 1889), have been re-collecetd by M. K n e z (1996).

All geological bibliography concerning Slovenian an Italian part of Kras is compiled in the papers of P a v l o v e c et al. (1989) and M a r t i n i s (1989).

G. S t a c h e (1880, 1889) described 7 genera and 18 species, 17 species and subspecies were new, of Lagynophoreae and Characeae families from these deposits.

The Maastrichtian sediments from Gavrovo (External Hellenids) and from Peloponesus peninsula contain R. liburnica, and they continuously pass into Paleocene sediments with textulariids, valvulinids, complex miliolids, and glomalveolinids (T s a i l a - M o n o p o l i s, 1977; F l e u r y, 1980; Z a m b a t a k i s - L e k k a, 1988; M a u r i k a s, 1993).

T ype 13X, 250/350 >ISO_7>ě>ISO_1>m (45/60 mesh), 1220 mm length × 2,16 mm ID shall be used and conditioned at least 12 h at 423 K (150 °C) with carrier gas prior to initial use.

In the Trieste Karst, the equivalent strata were termed the Opicina member (C u c c h i et al., 1989, Pl.1,2), and nummulitic-alveolinal limestone in the Soča Karst (Calcari a nummuliti e alveoline, Te n t o r et al., 1994).

G. S t a c h e (1889) was the first who studied Paleocene carbonate rocks and named them collectively the " Liburnia stage " (Liburnische Stufe) after the Liburnia area along the Adriatic coast, between the rivers of Raša and Krka.

In order to shed more light on specific sedimentologic conditions during the formation of the Liburnia deposits, G. S t a c h e (1889, p. 125) gave the lists of detailed descriptions of areas with living characeans from the South America, Africa and Mediterranean. G r a m b a s t (1971) and later researchers studied Characeans from Pyrenean basin, Paris basin and Liburnia deposits resulted in new taxonomy and biostratigraphic evaluation.

Surveys of Slovene public opinion assessed the attitude towards homosexuals using the scale of social distance (e.g. 'whom wouldn't you like to have as a neighbor?'), and on the basis of the respondents' views about sexual relations between two adult persons of the same sex.

The procuring entity is defined in Article 3 §2 and §3 of Act No. 263/1999 Z. z. on Public Pr ocurement, as amended, as a legal entity which deals in operating transport on the railways (Act No. 164/1996 Z. z. as amended, Act No. 258/1993 Z. z. as amended - e.g. Ţeleznice Slovenskej republiky, Ţelezničnį spoločnos ť a.s.)";

the headings "B. DENMARK", "C. GERMANY", "D. GREECE", "E. SPAIN", "F. FRANCE", "G. IRELAND", "H. ITALY", "I. LUXEMBOURG", "J. NETHERLANDS", "K. AUSTRIA", "L. PORTUGAL", "M. FINLAND", "N. SWEDEN" and "O. UNITED KINGDOM" become "C. DENMARK", "D. GERMANY", "F. GREECE", "G. SPAIN", "H. FRANCE", "I. IRELAND", "J. ITALY", "N. LUXEMBOURG", "Q. NETHERLANDS", "R. AUSTRIA", "T. PORTUGAL", "W. FINLAND", "X. SWEDEN" and "Y. UNITED KINGDOM";

the headings "B. DENMARK", "C. GERMANY", "D. SPAIN", "E. FRANCE", "F. GREECE", "G. IRELAND", "H. ITALY", "I. LUXEMBOURG", "J. NETHERLANDS", "K. AUSTRIA", "L. PORTUGAL", "M. FINLAND", "N. SWEDEN" and "O. UNITED KINGDOM" are reordered with their respective entries and become "C. DENMARK", "D. GERMANY", "F. GREECE", "G. SPAIN", "H. FRANCE", "I. IRELAND", "J. ITALY", "N. LUXEMBOURG", "Q. NETHERLANDS", "R. AUSTRIA", "T. PORTUGAL", "W. FINLAND", "X. SWEDEN" and "Y. UNITED KINGDOM";

Toetust makstakse... tonni puhul (kogus, mille kohta on litsents välja antud). - >ISO_7>ÅðéóôñïöÞ éó÷ýïõóá ãéá... ôüíïõò (ðïóüôçôá ãéá ôçí ïðïßá Ý÷åé åêäïèåß ôï ðéóôïðïéçôéêü) - >ISO_1>Refund valid for... tons (quantity for which the licence is issued) - Restitution valide pour... tonnes (quantité pour laquelle le certificat est délivré) - Restituzione valida per... t (quantitativo per il quale il titolo è stato rilasciato) - Kompensacija paredzeta... t (daudzums, attieciba uz ko ir izsniegta atlauja) - Grazinamoji ismoka taikoma... tonoms (kiekis, kuriam isduota licencija) - A visszatérítés... tonnára érvényes (az a mennyiség, amelyre az engedélyt kiállították) - Rifuzjoni valida gal... tunnellata (kwantità li galiha gie marug ic-certifikat) - Restitutie geldig voor... ton (hoeveelheid waarvoor het certificaat wordt afgegeven) - Refundacja wazna dla... ton (ilosc, dla której pozwolenie zostao wydane) - Restituição válida para... toneladas (quantidade relativamente à qual é emitido o certificado) - Náhrada platná pre... ton (mnozstvo, na ktoré sa povolenie vydáva) - Nadomestilo veljavno za... ton (kolicina, za katero je bilo izdano dovoljenje) - Tuki on voimassa... tonnille (määrä, jolle todistus on myönnetty) - Ger rätt till exportbidrag för... ton (den kvantitet för vilken licensen utfärdats)."

N o t e

T ę te de Moine: