Zobrazeno 1 - 10
of 80
pro vyhledávání: '"F.I. Zhimulev"'
Publikováno v:
Russian Geology and Geophysics. 64:558-570
—The Salair fold-thrust orogenic belt (Salair orogen, Salair) is located in the northwestern Altai–Sayan fold area within the Central Asian Orogenic Belt. The Salair orogen is an allochthon overriding the Kuznetsk Basin on a system of imbricate t
Autor:
E.V. Vetrov, A.N. Uvarov, E.S. Andreeva, N.I. Vetrova, F.I. Zhimulev, A.S. Stepanov, I.A. Vishnevskaya, M.V. Chervyakovskaya
Publikováno v:
Russian Geology and Geophysics. 63:1333-1353
—The Tuvinian trough is one of the large grabens of the rift system formed in the Devonian–Carboniferous in the eastern part of the Altai–Sayan fold area. Based on the results of comprehensive studies, the age was refined, and the geochemical f
Publikováno v:
Russian Geology and Geophysics. 63:1-12
—Neotectonic activity in the area of the Salair Ridge (southern West Siberia) rejuvenated a system of large arc-shaped faults separating the Salair tectonic arc from the adjacent tectonic units. These regional faults, which make up the general tect
Autor:
E.V. Vetrov, F.I. Zhimulev, S.A. Dokashenko, G. Van Ranst, I.S. Novikov, Simon Nachtergaele, J. De Grave
Publikováno v:
Russian Geology and Geophysics. 62:1006-1020
—The Kolyvan’–Tomsk folded zone (KTFZ) is a late Permian collisional orogen in the northwestern section of the Central Asian Orogenic Belt. The Mesozoic history of the KTFZ area includes Late Triassic–Early Jurassic and Late Jurassic–Early
Autor:
E. F. Letnikova, N. K. Danukalov, Andrey A. Tretyakov, V. P. Kovach, Hao-Yang Lee, Kirill E. Degtyarev, F.I. Zhimulev, N. A. Kanygina
Publikováno v:
Geotectonics. 54:605-627
This work presents the results of a study of metamorphic rocks of the Bekturgan and Balazhezdy groups of the Precambrian Ulutau massif (Central Kazakhstan), which have been traditionally identified with the most ancient Early Precambrian complexes, c
Publikováno v:
Geological Journal. 55:1913-1930
The Kolyvan-Tomsk folded zone (KTFZ) represents part of the Central Asian Orogenic Belt (CAOB). The KTFZ is mainly composed of detrital Late Palaeozoic sedimentary deposits, with minor intrusions. Detrital zircon geochronology on the Upper Devonian t
Autor:
N. I. Vetrova, F.I. Zhimulev, A. N. Uvarov, Geochemistry Ub Ras, M.V. Chervyakovskaya, I. A. Vishnevskaya, Mineralogy Sb Ras, E.V. Vetrov, E. S. Andreeva
Publikováno v:
Geology and mineral resources of Siberia. :81-94
Autor:
Jack Gillespie, Gilby Jepson, F.I. Zhimulev, Martin Danišík, Stijn Glorie, Dmitriy Gurevich, Alan S. Collins
Publikováno v:
Journal of the Geological Society. 178
Central Asia hosts the Tianshan, the largest intracontinental mountain belt in the world, which experienced major reactivation and uplift since the Oligocene in response to the collision of India with Asia. This reactivation was focused around pre-ex
Autor:
Wenjiao Xiao, F.I. Zhimulev, Martin Danišík, Zhiyong Zhang, Jack Gillespie, Gilby Jepson, A. Otasevic, Dongfang Song, D. Gurevich, Stijn Glorie
Publikováno v:
Geoscience Frontiers, Vol 10, Iss 6, Pp 2153-2166 (2019)
The Junggar Alatau forms the northern extent of the Tian Shan within the Central Asian Orogenic Belt (CAOB) at the border of SE Kazakhstan and NW China. This study presents the Palaeozoic–Mesozoic post-collisional thermo-tectonic history of this fr
Publikováno v:
Russian Geology and Geophysics. 60:781-792
—Middle Mesozoic and Cenozoic tectonic events on the periphery of the West Siberian Plain and in the flanking mountains of the northwestern Altai–Sayan province produced highland topography over a part of southeastern West Siberia. The activity s