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| LEADER |
01850ntm a22004817i 4500 |
| 001 |
MUB01006440854 |
| 003 |
CZ BrMU |
| 005 |
20200313135434.0 |
| 008 |
190410s1955 xr ||||| |||||||||||cze d |
| STA |
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|a POSLANO DO SKCR
|b 2020-04-14
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| 040 |
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|a BOD004
|b cze
|e rda
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| 041 |
1 |
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|a cze
|h eng
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| 072 |
|
7 |
|a 624
|x Stavební inženýrství
|2 Konspekt
|9 19
|
| 080 |
|
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|a 628.112
|2 MRF
|
| 080 |
|
|
|a 624.131.34:556.3
|2 MRF
|
| 080 |
|
|
|a (0.036.6)
|2 MRF
|
| 100 |
1 |
|
|a Hantush, Mahdi S.,
|d 1921-1984
|4 aut
|
| 240 |
1 |
0 |
|a Steady three-dimensional flow to a well in a two -layered aquifer
|
| 245 |
1 |
0 |
|a Ustálený trojrozměrný přítok vody k vrtu v dvojité zvodnělé vrstvě /
|c Mahdi S. Hantush - C.E Jacob
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| 264 |
|
0 |
|c [1955?]
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| 300 |
|
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|a 7 volných listů
|
| 336 |
|
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|a text
|b txt
|2 rdacontent
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| 337 |
|
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|a bez média
|b n
|2 rdamedia
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| 338 |
|
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|a svazek
|b nc
|2 rdacarrier
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| 500 |
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|a Překlad článku
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| 650 |
0 |
7 |
|a hydrogeologické vrty
|7 ph931390
|2 czenas
|
| 650 |
0 |
7 |
|a studny
|7 ph116306
|2 czenas
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| 650 |
0 |
9 |
|a hydrogeological boreholes
|2 eczenas
|
| 650 |
0 |
9 |
|a wells
|2 eczenas
|
| 655 |
|
7 |
|a separáty
|7 fd131867
|2 czenas
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| 655 |
|
9 |
|a offprints
|2 eczenas
|
| 700 |
1 |
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|a Jacob, C. E.
|4 aut
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| 787 |
0 |
8 |
|i Separát z:
|t Americal Geophysical Union Transaction
|g 36 (1955)
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| CAT |
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|a DRIMLOVA
|b 02
|c 20190410
|l MUB01
|h 1145
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| CAT |
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|a CHYTKOVA
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|c 20200313
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| CAT |
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|c 20200414
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| CAT |
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|c 20210614
|l MUB01
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| CAT |
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|c 20210614
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|h 2019
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| CAT |
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|a BATCH
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|c 20210724
|l MUB01
|h 1310
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| LOW |
|
|
|a POSLANO DO SKCR
|b 2020-04-14
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| 994 |
- |
1 |
|l MUB01
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|2 PRSGL
|b ÚK sklad - GL
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|4 dar Pelikán
|8 20190410
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|r 20190410
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| AVA |
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|a SCI50
|b PRIF
|c ÚK sklad - GL
|d I-37843
|e available
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