|
|
|
|
LEADER |
01168nab#a2200349#ar4500 |
001 |
000000991 |
003 |
SVKKK |
005 |
00000000000000.0 |
008 |
c xo e engo |
FMT |
|
|
|
038 |
|
|
|a SVKKK
|
040 |
|
|
|a SVKKK
|b slo
|e AACR2
|
041 |
0 |
|
|a eng
|b eng
|
044 |
|
|
|a xo
|c SK
|
080 |
|
|
|a 550.
|2 1981
|
080 |
|
|
|a 552.32
|2 1981
|
100 |
1 |
|
|a Orlický, Oto
|4 aut
|
242 |
1 |
0 |
|a Curierove teploty Fe-TI oxidov čadičov: je možné použitie curierovej teploty na stanovenie pôvodu Fe-Ti oxidov a príbuzného magmatického čadiča?
|
245 |
1 |
0 |
|a Curie temperatures of the Fe-Ti oxides of basalts: Is it posible to use Curie temperatures to assess the source or the depth of the Fe-Ti oxides and related basalt magmas?
|c Orlický Oto,
|
300 |
|
|
|b Obr. 4, tab. 1,
|
504 |
|
|
|a Res. angl., lit. 22 zázn. v angl.
|
650 |
0 |
4 |
|a titanomagnetity
|x horniny vyvrelé
|x Curierova teplota
|x štúdie
|
650 |
0 |
4 |
|a čadiče
|
773 |
0 |
|
|t Geologica Carpathica
|x 1335-0552
|g Roč. 47, č. 1(1996), s. 51-58
|
958 |
|
|
|a MS
|
958 |
|
|
|a NB
|
958 |
|
|
|a NP
|
974 |
|
|
|d 960607
|a 244
|
992 |
|
|
|a RBX
|
BAS |
|
|
|
852 |
|
|
|a SVKKK
|b BIB
|
998 |
|
|
|a GEO
|