geologie
| Field | Ind | Field content |
| leader | -----cz a22--------4500 | |
| 1 | ph114622 | |
| 3 | CZ PrNK | |
| 5 | 20180405044027.4 | |
| 8 | 000804|n|anznnbabn n a|a | |
| 40 | ## | $a ABA001 $b cze $d ABA001 |
| 72 | #7 | $a 55 $x Vědy o Zemi. Geologické vědy $2 Konspekt $9 7 |
| 80 | $a 55 $2 MRF_2003 | |
| 150 | $a geologie $7 ph114622 | |
| 550 | $a geokryologie $7 ph849164 | |
| 550 | $a geologická kartografie $7 ph120526 | |
| 550 | $a geologické informace $7 ph120527 | |
| 550 | $a geologické sbírky $7 ph628374 | |
| 550 | $a geologické vědy $7 ph120530 | |
| 550 | $a geologové $7 ph120533 | |
| 550 | $a geoložky $7 ph895138 | |
| 550 | $a geoparky $7 ph502996 | |
| 550 | $a geostatistika | |
| 550 | $w h $a aplikovaná geologie $7 ph134717 | |
| 550 | $w h $a dějiny geologie $7 ph484328 | |
| 550 | $w h $a environmentální geologie $7 ph184842 | |
| 550 | $w h $a fyzikální geologie $7 ph120436 | |
| 550 | $w h $a geobiologie $7 ph134796 | |
| 550 | $w h $a geochemie $7 ph120501 | |
| 550 | $w h $a geochronologie $7 ph120502 | |
| 550 | $w h $a geofyzika $7 ph114615 | |
| 550 | $w h $a geologický vývoj Země $7 ph242459 | |
| 550 | $w h $a geomorfologie $7 ph114625 | |
| 550 | $w h $a glaciální geologie $7 ph120565 | |
| 550 | $w h $a historická geologie $7 ph114666 | |
| 550 | $w h $a izotopová geologie $7 ph121257 | |
| 550 | $w h $a karsologie $7 ph138653 | |
| 550 | $w h $a kosmická geologie $7 ph134858 | |
| 550 | $w h $a matematická geologie $7 ph691047 | |
| 550 | $w h $a mořská geologie $7 ph124159 | |
| 550 | $w h $a obecná geologie $7 ph323329 | |
| 550 | $w h $a regionální geologie $7 ph125075 | |
| 550 | $w h $a seizmologie $7 ph116120 | |
| 550 | $w h $a speleologie $7 ph125905 | |
| 550 | $w h $a stratigrafie $7 ph126131 | |
| 550 | $w h $a strukturní geologie $7 ph126152 | |
| 550 | $w h $a tektonika $7 ph116414 | |
| 550 | $w g $a vědy o Zemi $7 ph127381 | |
| 550 | $a geostatistika $7 ph120544 | |
| 750 | $a geology $2 eczenas | |
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| 906 | $a wu20141127 $b napo | |
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| 998 | $a 000114622 |