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Trofimuk Institute of Petroleum-Gas Geology and Geophysics of the Siberian Branch of the RAS, IPGG SB RAS (Russian: Институт нефтегазовой геологии и геофизики имени А. А. Трофимука СО РАН, ИНГГ СО РАН) is a research institute in Novosibirsk, Russia. It was founded in 2005.
The main activities of service: basic research and applied research in the field of seismology and geophysics, as well as conducting continuous seismic monitoring of the Russian Federation, tsunami warning in the Russian Far East, monitoring volcanic activity in Kamchatka and slow monitoring of geodynamic processes in the crust and ground deformation, carrying out continuous seismic monitoring ...
Siberian Research Institute of Geology, Geophysics and Mineral Resource; Established: 1957: Director: Mikhail Epov: ... Geophysics and Mineral Resources (Russian: ...
Several hundred children aged 10 to 17 from 46 regions of Russia and foreign countries have already taken part in the project. During GeoArtek, young geologists are trained in methods of geological field researches, safety rules during expeditions, and acquaintance with environmental problems.
The geology of Russia, the world's largest country, which extends over much of northern Eurasia, consists of several stable cratons and sedimentary platforms bounded by orogenic (mountain) belts. European Russia is on the East European craton , at the heart of which is a complex of igneous and metamorphic rocks dating back to the Precambrian .
Geologic formations of Russia (2 C, 31 P) Fossils of Russia (3 C, 329 P) G. ... Pages in category "Geology of Russia" The following 36 pages are in this category, out ...
Petroleum Field Geology; Geology; Geophysical Information Systems; Exploration Geophysics and Computer Systems; lithology and System Research of Lithosphere; Geology of Hydrocarbon Systems; Aleksandr V. Lobusev is author of more than 90 scientific papers. He is also the holder of the patent: "Method of developing oil and gas fields”.
Step-like geomorphology at the Putorana Plateau, which is a World Heritage Site.. The source of the Siberian Traps basaltic rock has been attributed to a mantle plume, which rose until it reached the bottom of the Earth's crust, producing volcanic eruptions through the Siberian Craton. [8]