Zobrazeno 1 - 10
of 13
pro vyhledávání: '"M. K. Danukalova"'
Autor:
A. B. Kuzmichev, M. K. Danukalova
Publikováno v:
Геодинамика и тектонофизика, Vol 15, Iss 2 (2024)
The article unravels a confusing history of ideas about the age of the Garevka granite pluton, which is considered as a reference object for the Precambrian of the Yenisei ridge. Initially, the Paleoproterozoic (1750 Ma) age of granite was determined
Externí odkaz:
https://doaj.org/article/d982687d8d154f818b1945906bc42bda
Autor:
A. B. Kuzmichev, M. K. Danukalova, V. F. Proskurnin, A. A. Bagaeva, N. I. Beresyuk, P. A. Gromov
Publikováno v:
Геодинамика и тектонофизика, Vol 10, Iss 4, Pp 841-861 (2019)
Eastern part of the Central Taimyr belt is composed of Precambrian rocks penetrated by granites of the Snezhnaya complex (845–825 million years) and later overlain by mid‐Neoproterozoic sin‐ postorogenic sedimentary deposits of the Stanovaya‐
Externí odkaz:
https://doaj.org/article/d7977839509a411ebbb3233733091b78
Publikováno v:
Lithology and Mineral Resources. 57:44-61
Publikováno v:
Paleontological Journal. 55:259-271
Permian marine bivalves of the Pronchishchev Ridge (North Siberia) were systematically studied for the first time.. The presence of the Middle and Upper Permian with five biostratigraphic levels was established based on fossil findings. In the Middle
Autor:
Yu. A. Gatovsky, Olga L. Kossovaya, V. G. Ganelin, Alexander B. Kuzmichev, T. N. Isakova, N. G. Astashkin, M. K. Danukalova, V. V. Eriklintsev, D. Weyer
Publikováno v:
Stratigraphy and Geological Correlation. 27:729-782
The information on the Late Palaeozoic deposits of the New Siberian Islands is essential to clarify the palaeogeography of the surrounding Arctic Region and to quest the original location of the New Siberian continental block prior to the Amerasian o
Autor:
M. K. Danukalova, G. N. Aleksandrova, V. B. Khubanov, Victor Zakharov, B.L. Nikitenko, E. V. Korostylev, Alexander B. Kuzmichev, Alexei B. Herman
Publikováno v:
Stratigraphy and Geological Correlation. 26:403-432
The model of geological structure of sedimentary cover of the Laptev Sea accepted by most geologists suggests that the lower seismic complex of the cover begins by the Aptian–Albian sedimentary rocks. They can be studied in natural outcrops of Kote
Autor:
A. A. Suyarkova, L. M. Melnikova, Alexander B. Kuzmichev, Peep Männik, N. P. Kul’kov, M. K. Danukalova, T. Yu. Tolmacheva
Publikováno v:
Stratigraphy and Geological Correlation. 23:468-494
Much of the material of Paleozoic successions of Kotelnyi Island (New Siberian Islands) is composed of various carbonates, which accumulated in relatively shallow conditions in the Ordovician–Middle Devonian. Such deposits are widespread in synchro
Publikováno v:
Journal of the Geological Society. 172:1-4
U–Pb detrital zircon results from New Siberian Islands sandstones illuminate the long-lived controversy regarding the continuation of the Uralian orogen into the Arctic region. A dominant age peak of c . 285 Ma from Permian sandstone requires proxi
Autor:
L. M. Melnikova, M. K. Danukalova
Publikováno v:
Paleontological Journal. 48:471-483
Ostracodes from the Middle-Upper Ordovician deposits (Malodiring-Ayan, Teryutekh, and Anisin formations) of Kotel’nyi Island are studied in detail for the first time. Brief descriptions of Ordovician localities on the Tuor-Yuryakh and Kazarka river
Publikováno v:
Geotectonics. 48:390-412
The archipelago of New Siberian Islands situated on the northeastern continental shelf of Eurasia is considered a part of an exotic terrane that collided with Siberia in the Early Cretaceous. Bel’kov Island is located close to the inferred western