Zobrazeno 1 - 6
of 6
pro vyhledávání: '"A. L. Anfimov"'
Publikováno v:
Литосфера, Vol 0, Iss 4, Pp 43-61 (2015)
Several reef-building systems occurred during Cambrian-Devonian on the Urals and adjacent regions of the East-European Platform. The first phase was manifested in the Lower Cambrian within a limited area of the western slope of the Urals. The next st
Externí odkaz:
https://doaj.org/article/67e0a18c7ad649818f09abc9f72c7ad8
Autor:
A. L. Anfimov
Publikováno v:
Литосфера, Vol 0, Iss 3, Pp 57-68 (2015)
The article highlights the following stages of the development microscopic Devonian Algae in the Urals: the rise of Algae in the early Devonian (Karpinski time), degradation of Algae flora during the end of Early Devonian (taltiysk time), the Middle
Externí odkaz:
https://doaj.org/article/43f1e14e0c63485da89045e910a57470
Autor:
A. L. Anfimov
Publikováno v:
Paleontological Journal. 46:445-452
Four new foraminiferal species, Parathuramminites mutilatus sp. nov., P. stelliformis sp. nov., P. subrus sp. nov., and P. minutus sp. nov., and a new genus and species, Algaeformis porosus gen. et sp. nov. from clayey limestones and marls of the bas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8b3f51212230bafb55f6220cac8d889b
https://doi.org/10.1134/s0031030112050024
https://doi.org/10.1134/s0031030112050024
Autor:
B. I. Chuvashov, A. L. Anfimov
Publikováno v:
Paleontological Journal. 41:95-102
The history of the genus Ungdarella and the family Ungdarellaceae is discussed. Data on thallus morphology in members of the family are analyzed. Three new genera, Ungdarelloides, Urtasimella, and Suundukella, and a new species of the genus Ungdarell
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5e969460e39f032a9802c76d202ab1a
https://doi.org/10.1134/s0031030107010108
https://doi.org/10.1134/s0031030107010108
Publikováno v:
Doklady Earth Sciences. 439:1076-1078
The Saf’yanovka copper massive sulfide deposit is situated 10 km northeast from the town of Rezh, on the eastern slope of the Central Urals. The ore-hosting plagiorhyolite-dacitic sequence consists of tephrites and tuffites with interlayers of dark
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::de85f74d35a1257e7b7a1995528086e1
https://doi.org/10.1134/s1028334x11080125
https://doi.org/10.1134/s1028334x11080125
Autor:
A. L. Anfimov, B. I. Chuvashov
Publikováno v:
Lithology and Mineral Resources. 36:211-223
During the Moscovian Age, the eastern part of the Russian Platform was occupied by the shallow-water East European Basin (EEB) characterized by predominantly carbonate sedimentation. In the Cis-Ural region of this basin, the deep Cis-Ural Sea (CUS) o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::951533e1297aad0707290997d908e830
https://doi.org/10.1023/a:1010473207620
https://doi.org/10.1023/a:1010473207620