The deep structures of the junction of the Urals with the Russian and West Siberian Platforms
A new model of the junction of the Ural fold belt with the Russian and West Siberian Platforms along the Europrobe Seismic Reflection profiling in the Urals (ESRU) down to a depth of 15 km is constructed. 2Dmodeling of the density and magnetic properties was performed using seven profiles and was ac...
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| Veröffentlicht in: | Doklady earth sciences 2017-07, Vol.475 (1), p.731-735 |
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| creator | Ivanov, K. S. Koroteev, V. A. Kostrov, N. P. |
| description | A new model of the junction of the Ural fold belt with the Russian and West Siberian Platforms along the Europrobe Seismic Reflection profiling in the Urals (ESRU) down to a depth of 15 km is constructed. 2Dmodeling of the density and magnetic properties was performed using seven profiles and was accompanied by an estimate of applicability of the method. In the west, the upper part of the model is represented by terrigeneous- carbonate deposits, and the bottom part shows the structures of the basement of the Russian platform, which becomes thinner eastward and plunges beneath the Ural structures. The most significant difference in the West Siberian part of the transect is the great “length” of the entire structure of the Earth’s crust. This is caused by the Early Triassic extension accompanied by the formation of a system of Triassic graben-rifts. |
| doi_str_mv | 10.1134/S1028334X17070042 |
| format | Article |
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S. ; Koroteev, V. A. ; Kostrov, N. P.</creator><creatorcontrib>Ivanov, K. S. ; Koroteev, V. A. ; Kostrov, N. P.</creatorcontrib><description>A new model of the junction of the Ural fold belt with the Russian and West Siberian Platforms along the Europrobe Seismic Reflection profiling in the Urals (ESRU) down to a depth of 15 km is constructed. 2Dmodeling of the density and magnetic properties was performed using seven profiles and was accompanied by an estimate of applicability of the method. In the west, the upper part of the model is represented by terrigeneous- carbonate deposits, and the bottom part shows the structures of the basement of the Russian platform, which becomes thinner eastward and plunges beneath the Ural structures. The most significant difference in the West Siberian part of the transect is the great “length” of the entire structure of the Earth’s crust. 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S.</creatorcontrib><creatorcontrib>Koroteev, V. A.</creatorcontrib><creatorcontrib>Kostrov, N. P.</creatorcontrib><title>The deep structures of the junction of the Urals with the Russian and West Siberian Platforms</title><title>Doklady earth sciences</title><addtitle>Dokl. Earth Sc</addtitle><description>A new model of the junction of the Ural fold belt with the Russian and West Siberian Platforms along the Europrobe Seismic Reflection profiling in the Urals (ESRU) down to a depth of 15 km is constructed. 2Dmodeling of the density and magnetic properties was performed using seven profiles and was accompanied by an estimate of applicability of the method. In the west, the upper part of the model is represented by terrigeneous- carbonate deposits, and the bottom part shows the structures of the basement of the Russian platform, which becomes thinner eastward and plunges beneath the Ural structures. The most significant difference in the West Siberian part of the transect is the great “length” of the entire structure of the Earth’s crust. 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| subjects | Carbonates Earth Earth and Environmental Science Earth crust Earth Sciences Earthquake construction Geology Graben Length Magnetic properties Magnetism Minerals Mountains Platforms Profiles Profiling Seismic reflection profiling Seismic surveys Structures Triassic |
| title | The deep structures of the junction of the Urals with the Russian and West Siberian Platforms |
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