| nr |
titel |
auteur |
tijdschrift |
jaar |
jaarg. |
afl. |
pagina('s) |
type |
| 1 |
AUTHORS' ABSTRACTS OF MOIP DOKLADY
|
|
|
1976
|
18 |
4 |
p. 475-494
|
artikel
|
| 2 |
Comparability of geochronological measurements of coexistent (coeval) minerals, made with different values of decay constants of K40, Rb87, and other radioactive elements1
|
Afanas'yev, G. D.
|
|
1976
|
18 |
4 |
p. 389-396
|
artikel
|
| 3 |
Dissipation of transmitted waves in thin-layered media
|
Kondrat'yeva, O. K.
|
|
1976
|
18 |
4 |
p. 462-474
|
artikel
|
| 4 |
Distribution of boron in rock-forming skarn minerals from (n,α)-radiography data
|
Berzina, I. G.
|
|
1976
|
18 |
4 |
p. 425-429
|
artikel
|
| 5 |
Distribution patterns of mineral resources in the Siberian Platform cover
|
Malich, N. S.
|
|
1976
|
18 |
4 |
p. 417-424
|
artikel
|
| 6 |
Features of the wave pattern associated with the Mohorovicic discontinuity in the Caucasus
|
Krasnopevtseva, G. V.
|
|
1976
|
18 |
4 |
p. 455-456
|
artikel
|
| 7 |
Microstructure of obsidian, using electron microscopy data
|
Nasedkin, V. V.
|
|
1976
|
18 |
4 |
p. 457-461
|
artikel
|
| 8 |
Neotectonic movements in the upper reaches of the Kolyma River
|
Betyakov, L. P.
|
|
1976
|
18 |
4 |
p. 445-449
|
artikel
|
| 9 |
Origin of increased amounts of elements in pelagic sediments of the oceans
|
Strakhov, N. M.
|
|
1976
|
18 |
4 |
p. 406-416
|
artikel
|
| 10 |
Problem of mutual relationships between the deep-seated Paleozoic structures of Southern Tien Shan and the buried Tadzhik-Afghan Massif
|
Portnyagin, E. A.
|
|
1976
|
18 |
4 |
p. 450-454
|
artikel
|
| 11 |
Quantitative estimation of temperature and geological time as factors in carbonification of disseminated coal residues, and possible applications in oil geology
|
Karpov, P. A.
|
|
1976
|
18 |
4 |
p. 397-405
|
artikel
|
| 12 |
Ring and tectonic faults in the Kyzyl-Ompul pluton
|
Nevskiy, V. A.
|
|
1976
|
18 |
4 |
p. 430-444
|
artikel
|
| 13 |
The oldest rocks of Antarctica (Enderby Land)
|
Sobotovich, E. V.
|
|
1976
|
18 |
4 |
p. 371-388
|
artikel
|
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