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20221004142022.0 |
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220614s1964 xxu||||| |||||||||||eng d |
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|a POSLANO DO SKCR
|b 2022-09-26
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| 040 |
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|a BOD004
|b cze
|e rda
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| 072 |
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7 |
|a 551
|x Geologie. Meteorologie. Klimatologie
|2 Konspekt
|9 7
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| 080 |
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|a 551.7
|2 MRF
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| 080 |
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|a 551.243
|2 MRF
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| 080 |
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|a 551.4.035
|2 MRF
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| 080 |
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|a 551.1/.4
|2 MRF
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| 080 |
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|a (738.7)
|2 MRF
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| 080 |
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|a (738.6)
|2 MRF
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| 080 |
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|a (738.3)
|2 MRF
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| 080 |
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|a (048.8)
|2 MRF
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| 100 |
1 |
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|a Robinson, Charles Sherwood,
|d 1920-
|7 jx20080310015
|4 aut
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| 245 |
1 |
0 |
|a Stratigraphy and structure of the northern and western flanks of the Black Hills uplift, Wyoming Montana, and South Dakota /
|c by Charles S. Robinson, William J. Mapel and Maximilian H. Bergendahl
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| 264 |
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1 |
|a Washington :
|b United States Government Printing Office,
|c 1964
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| 300 |
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|a iv, 134 stran +
|e 6 složených listů (mapy, diagramy)
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| 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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| 490 |
1 |
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|a Geological Survey professional paper ;
|v 404
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| 504 |
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|a Obsahuje bibliografii a rejstřík
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| 650 |
0 |
7 |
|a stratigrafie
|7 ph126131
|2 czenas
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| 650 |
0 |
7 |
|a strukturní geologie
|7 ph126152
|2 czenas
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| 650 |
0 |
7 |
|a pohoří
|7 ph124196
|2 czenas
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| 650 |
0 |
7 |
|a regionální geologie
|7 ph125075
|2 czenas
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| 650 |
0 |
9 |
|a stratigraphy
|2 eczenas
|
| 650 |
0 |
9 |
|a structural geology
|2 eczenas
|
| 650 |
0 |
9 |
|a mountain range
|2 eczenas
|
| 650 |
0 |
9 |
|a regional geology
|2 eczenas
|
| 651 |
|
7 |
|a Wyoming
|7 ge134591
|2 czenas
|
| 651 |
|
7 |
|a Montana
|7 ge134373
|2 czenas
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| 651 |
|
7 |
|a Jižní Dakota
|7 ge128488
|2 czenas
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| 651 |
|
9 |
|a Wyoming
|2 eczenas
|
| 651 |
|
9 |
|a Montana
|2 eczenas
|
| 651 |
|
9 |
|a South Dakota
|2 eczenas
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| 655 |
|
7 |
|a studie
|7 fd133597
|2 czenas
|
| 655 |
|
9 |
|a studies
|2 eczenas
|
| 700 |
1 |
|
|a Mapel, W. J.
|q (William Jameson),
|d 1922-
|7 jx20050726006
|4 aut
|
| 700 |
1 |
|
|a Bergendahl, Maximilian Hilmar,
|d 1921-
|4 aut
|
| 830 |
|
0 |
|a Geological Survey professional paper ;
|v 404
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