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1.
Vernikovskaya A. E. Vernikovsky V. A. Matushkin N. Yu. Kadilnikov P. I. Metelkin D. V. Li Z.-X. Wilde S. A. Romanova I. V. Bogdanov E. A. 《Doklady Earth Sciences》2019,489(1):1285-1288
Doklady Earth Sciences - An Ediacaran complex of dike rocks has been identified for the first time in the Yenisei Ridge orogen. These igneous rocks are represented by basic, intermediate and acidic... 相似文献
2.
V. V. Abashev D. V. Metelkin N. E. Mikhal’tsov V. A. Vernikovsky N. Yu. Matushkin 《Izvestiya Physics of the Solid Earth》2017,53(5):677-694
The rock magnetic and paleomagnetic results from the Upper Paleozoic sedimentary sequences composing the isles of the Novaya Zemlya Archipelago are presented. The recorded temperature dependences of the magnetic susceptibility, the magnetic hysteresis parameters, and the results of the first-order reversal curve (FORC) measurements suggest the presence of single-domain or pseudo-single-domain magnetite and hematite grains in the rocks. The Upper Paleozoic deposits overall are promising for unraveling the tectonic evolution of the Barents–Kara region. Together with the rock magnetic data, the positive fold and reversal tests testify to the primary origin of the indentified magnetization components. However, the interpretation of the paleomagnetic data should take into account the probable inclination shallowing. New substantiation is offered for the paleomagnetic poles for Early Devonian and Late Permian. For the first time, paleomagnetic constraints are obtained for the Late Carboniferous boundary. It is shown that the Early Cimmerian deformation stage within the Paikhoi–Novaya Zemlya region is associated with the sinistral strike slip displacement along the Baidaratskii suture during which the internal structure of the Southern Novaya Zemlya segment could undergo shear in addition to the nappe-thrust transformations. The Northern Novaya Zemlya segment, which is shifted northwest with respect to the Southern segment, was deformed in the thrusting mode with an overall clockwise rotation of this segment relative to the East European Craton. 相似文献
3.
Metelkin D. V. Lavrenchuk A. V. Mikhaltsov N. E. 《Izvestiya Physics of the Solid Earth》2019,55(6):833-840
Izvestiya, Physics of the Solid Earth - The possibility of reconstructing geologic events by identifying patterns in variations of the geomagnetic field related to reversals is one of the... 相似文献
4.
V.A. Vernikovsky A.Yu. Kazansky N.Yu. Matushkin D.V. Metelkin J.K. Sovetov 《Russian Geology and Geophysics》2009,50(4):380-393
The formation of the western margin of the Siberian craton in the Neoproterozoic is considered, with a focus on its transformation from a passive continental margin into an active one, accretion and collision processes, formation of island arcs and ophiolites, orogeny, and continent-marginal rifting. The evolution and correlation of sedimentary basins within fold-thrust belts of the Siberian Platform framing are considered. New structural and kinematic data on the Yenisei fault zone are discussed. On the basis of paleomagnetic data obtained for the structures in the zone of junction of the Siberian Platform and the West Siberian Plate, new models are proposed for the location of the Siberian craton relative to other paleocontinents and microcontinents in the Neoproterzoic. All these data provide a consistent evolution scheme for the western margin of the Siberian paleocontinent in the Neoproterozoic and constrain the position of the Siberian craton margin in Late Neoproterozoic (pre-Vendian) time. 相似文献
5.
V. Yu. Timofeev A. Yu. Kazansky D. G. Ardyukov D. V. Metelkin P. Yu. Gornov N. V. Shestakov A. V. Timofeev G. Z. Gil’manova 《Russian Journal of Pacific Geology》2011,5(4):288-297
The motion of lithospheric blocks was analyzed in the junction zone between the Eurasian Plate and its surrounding structures.
Its present-day stage was considered using GPS and seismologic data. Models of the movement of a rigid plate are considered
for Eurasia. A model of Eurasia (northern part of Asia) was used to determine the rotation parameters of its southern periphery
(Amur Plate) based on GPS data for the Far East (Sikhote Alin profile), and Transbaikal regions are shown as an example. A
model of the Amur Plate was used to illustrate the behavior of the extension zone on its western boundary represented by the
Lake Baikal depression during the Kultuk earthquake (M = 6.3, August, 27, 2008). Paleomagnetic data made it possible to determine
the rotation pole of the Siberian Craton relative to its surrounding folded structures during the Mesozoic and to estimate
its kinematic parameters. The permanent position of the rotation pole in the relative coordinate system since the terminal
Paleozoic until the Recent indicates a constant rotation velocity of the Siberian domain within the Eurasian Plate structure. 相似文献
6.
7.
Abashev V. V. Vernikovsky V. A. Kazansky A. Yu. Metelkin D. V. Mikhaltsov N. E. Bragin V. Yu. 《Doklady Earth Sciences》2019,486(1):481-484
Doklady Earth Sciences - The work presents the first results on the anisotropy of magnetic susceptibility in Hooker Island basaltoids; this anisotropy is related to the direction of motion of the... 相似文献
8.
We present paleomagnetic data on the Cambrian volcanosedimentary complexes of the Bateni Ridge, which correspond to the evolution of the Kuznetsk Alatau island arc. The paleomagnetic poles which served as the basis for the apparent polar-wander path (APWP) were determined. The paleomagnetic data were compared with those on the Cambrian poles for other fragments of the Kuznetsk Alatau island arc.For example, the APWP of the Bateni fragment corresponds to that of the Kiya (Martaiga) fragment of the eastern slope of the Kuznetsk Alatau. The distribution of the paleomagnetic poles suggests that the relative drift of the Kuznetsk Alatau arc fragments and the entire island arc system resulted from large-amplitude strike-slips. In the Cambrian, this paleoarc moved from ～10° N to ～10° S and rotated more than 50° clockwise. In the paleomagnetic record, its accretion is reflected in the coincidence of the Late Cambrian–Early Ordovician poles on the eastern slope of the Kuznetsk Alatau with one another and the coeval poles for the Siberian craton. This coincidence also suggests that the general structure of the present Kuznetsk Alatàu formed as early as the Early Caledonian. Nevertheless, the differences in the position of the poles on the western and eastern slopes of the Kuznetsk Alatau suggest that strike-slip activity along the Kuznetsk–Altai deep fault (the major one in the region) continued in the Late Paleozoic and, probably, in the Mesozoic. 相似文献
9.
D. V. Metelkin I. V. Gordienko L. I. Vetluzhskikh N. E. Mikhaltsov 《Doklady Earth Sciences》2013,449(1):284-289
We present new data on the geologic structure and paleomagnetism of the Vendian and Lower Cambrian deposits of the Argun River region in East Transbaikalia. We discuss the issues related to the recognition of the Argun microcontinent within the composite blocks of the south-eastern part of the Central Asian belt, which are traditionally combined in the Amuria superterrane. Our paleomagnetic determinations help us justify the equatorial position of the sedimentary basin, in which the deposits of the Argun terrane Beletuy and Bystrin formations formed 560 and 525 Ma, close to or directly on the margin of the Siberian paleocontinent. This data is essential for the reconstruction of the geodynamic evolution of Siberia and Central Asia at the Precambrian-Paleozoic boundary. 相似文献
10.
V. A. Vernikovsky D. V. Metelkin T. Yu. Tolmacheva N. A. Malyshev O. V. Petrov N. N. Sobolev N. Yu. Matushkin 《Doklady Earth Sciences》2013,451(2):791-797
The New Siberian Islands terrane, represented on the Arctic shelf by the archipelagos of the New Siberian Islands and De Long Islands, is one of the key structures of the Arctic. However many questions of its structure, borders and formation history are under intense discussion. During the international expedition in 2011 we solved many problems concerning structural geology, paleontology, petrology and geochronology. A particular attention was given to obtaining paleomagnetic data for the sedimentary and igneous rocks of the archipelago. The primary objects of paleomagnetic studies were the Early Paleozoic sedimentary rocks of the Kotelny (Anzhu) and Bennett (De Long) islands. In this paper we present new paleontological data, including the first one for conodonts of the New Siberian Islands, which help us to specify the age of the Early Paleozoic deposits of the studied sections. In these sections we took a series of paleomagnetic samples. The match of the paleomagnetic directions we determined for Bennett Isl. and Kotelny Isl. indicates the tectonic unity between the territories of the Anzhu and De Long archipelagos. These first paleomagnetic data allow us to affirm that at least from the Early Ordovician the rocks of the Anzhu and De Long archipelagos formed within the same New Siberian Islands terrane, that is to say, on the same basement. 相似文献