By Dennis Brown, Christopher Juhlin, Victor Puchkov
Published via the yankee Geophysical Union as a part of the Geophysical Monograph Series.
Extending for greater than 2000 kilometers from the islands of Novaya Zemlya within the north to the Aral Sea within the south, the Uralide orogen kinds the geographical and geological divide among Europe and Asia. For greater than a century the Uralides were one of many key parts of geological learn in Russia, and feature supplied a lot of its mineral and petroleum wealth for the final 50 years. however, the geology and tectonic evolution of the Uralide orogen have been quite unknown within the foreign literature until eventually lately, while EUROPROBE and GEODE (European technological know-how beginning medical programmes) introduced jointly Russian, ecu, and American earth scientists to paintings within the Uralides undertaking and the Urals Mineral Province undertaking, respectively. a lot of the new learn has centred round deep seismic surveys, Europrobe's Seismic mirrored image Profiling within the Urals (ESRU) survey within the center Urals and the multicomponent Urals Seismic test and built-in experiences (URSEIS) survey within the South Urals. those experiments have been observed through various geological, geochemical, geochronological, and geophysical studies.Content:
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Extra resources for Mountain Building in the Uralides: Pangea to the Present
Gorozhanina and D. Brown, Arc-Continent Collision in the Southern Urals: Petrogenetic Aspects of the Fore-Arc Complex, this volume. Tevelev, A. , I. A. Kosheleva and A. V. Ryazantsev, The composition and structural position of the Ordovician cherty basalt complexes of the Southern Urals (in Russian), in General and Regional Questions of Geology, 2, pp. 25^45, Geol. , Moscow, 2000. Timonin, N. , The Pechora Plate: The Geological History in the Phanerozoic (in Russian), edited by V. , Uralian branch of Russian Ac.
Puchkov, V. , The occurrences of Devonian conodonts at the western slope of the Urals and their importance for the stratigraphy of the Lemva-type Paleozoic (in Russian), in Conodonts of the Urals and Their Stratigraphic Significance, edited by G. Papulov and V. Puchkov, pp. 33-52, Inst. Geol. , Sverdlovsk, 1979b. Puchkov, V. , The place of intraplate events in the history of foldbelts (in Russian), in Intraplate Events in the Earth's Crust, pp. 167-175, Nauka, Moscow, 1988. Puchkov, V. , New data on the geology of the Sub-Kraka allochthonous complexes (Southern Urals) (in Russian), in Ezhegodnik-1994, pp.
I. Shalimov, Late Precambrian to Triassic history of the East-European craton: dynamics of sedimentary basin evolution, Tectono physics, 268, 23-63, 1996. Nikonov, N. , V. I. Bogatski, A. V. Martynov, Z. V. Larionova, V. M. Laskin, L. V. Galkina, E. G. Dovhikova, O. L. Ermakova, P. K. Kostygova, T. I. Kuranova, K. A. Moskalenko, Yu. A. Pankratov, E. L. Petrenko, E. V. Popova, A. I. Surina and G. A. Shabanova, Timan-Pechora Sedimentary Basin. Atlas of Geological Maps (in Russian), 64 sheets, Timan-Pechora Research Center, Ukhta, 2000.