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・ Murat Erdoğan
・ Murat Eriş
・ Murat Evliyaoğlu
・ Murat Gasaev
・ Murat Gomleshko
・ Murat Gülsoy
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Murat Kamaletdinov
・ Murat Karakoç
・ Murat Karayalçın
・ Murat Karayılan
・ Murat Kardanov
・ Murat Kaya
・ Murat Kaya (writer)
・ Murat Kayalı
・ Murat Khasanov
・ Murat Khotov
・ Murat Khrachev
・ Murat Kunt
・ Murat Kurnaz
・ Murat Köprülü
・ Murat Mukov


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Murat Kamaletdinov : ウィキペディア英語版
Murat Kamaletdinov

Kamaletdinov Murat Abdulhakovich (18 July 1928 — 1 July 2013) was a Bashkir petroleum geologist.
== Biography ==
Born on July 18, 1928 in Tomsk, Kamaletdinov Murat Abdulkhakovich graduated from Kazan State University in 1953. He began his career as a foreman at the geological prospecting expedition office in Sterlitamak city of Bashkir ASSR. Murat Abdulhakovich became the Chief of the geological party in 1955, then went on to head the geological expedition as Chief geologist of the Sterlitamak prospecting office.
In 1969, he worked at the Institute of Geology of the Bashkir Branch of the USSR, first as a senior researcher then in 1974 as head of the laboratory of Tectonics of the Institute of Geology of the Ural Scientific Center of Russian Academy of Sciences. After that in 1976 to 1991, Murat Abdulhakovich was the Director of the Institute of Geology of the Ural Scientific Center of the Russian Academy of Sciences .
From 1974 to 1997, M.A. Kamaletdinov conducted lectures at the Bashkir State University, during this period he became an academician of the Academy of Sciences of the Republic of Bashkortostan, an honorary member of the Academy of Natural Sciences (1997), a member of the Tectonic Committee of the USSR (1976–1991), and Honored Worker of Science and Technology of the Republic of Bashkortostan.
M.A. Kamaletdinov is a discoverer of the nappe tectonics of Urals. In 1954, when the Soviet Geology categorically denied nappes he first proved the existence of the large-scale Karatau nappe on the western slope of the Southern Urals. This discovery was followed by his findings of many other tectonic sheets and a large number of allochthonous outcrops in the South and Middle Urals, which before him were by mistake considered as anticlinal folds. This led to a radical revision of traditional fixists views and changed them to a new paradigm, which states the nappe structure of the Ural Mountains.
M.A. Kamaletdinov participated in the discovering Tabynsk, Romadanovsky, Voskresensky, Shabagishsky, Yermolayevsky, Torgassky, Teyruksky and other oil deposits of the PreUrals and developed a new effective method searching them. http://burneft.ru/archive/issues/2008-07-08/21
He created a geotectonic scientific school in which the horizontal movements of tectonic plates of the Earth's crust play a key role in its structure and history of development. Together with R.A. Kamaletdinov in 1971 he was the first to discover that the formation of foredeeps associated with isostatic dip edge of the continental platform under the weight of bearing down on them orogenic structures. Together with Yu.V. Kazantsev and T.T. Kazantseva,he made a comparative analysis of the tectonics of the Urals with the Crimea, the Caucasus, Pamir, Himalayas, Appalachians, the Rocky Mountains and other orogenic zones, the results of which allowed for the first time to conclude nappe-thrust structure of mountain belts of the world and their allochthonous occurrence on the continents. Forecast of prospects for oil and gas of undernappe zones was made. Together with D.V. Postnikov were studied foundations of ancient and young platforms: Eastern European, Western European, Siberian, West Siberian, North American, African. He found that they also
have nappe-thrust structure. Extensive data analysis revealed the existence of a genetic connection between allochthons and deposits, nappes and thrusts create conditions for the generation and for the accumulation of deposits. Thrusts were found on other terrestrial planets of the solar system, the similarities between modern development of the satellite Io of the planet Jupiter and revolutionary geological events in the Earth in the last era of its history were discovered. http://elibrary.ru/item.asp?id=18278398
All these data allowed M.A. Kamaletdinov to create a new global geological theory, which he called nappe-thrust. According to this theory, thrusts are the major structural elements of the stone shell of the planet, movements of thrusts cause main geological processes in the past and present: orogeny, folding, sedimentation, magmatism, metamorphism, seismicity, and the formation of important mineral resources (oil, gas, metal ores, diamonds and other minerals). This theory allowed to explain geological phenomena and processes in their cause-and-effect relationships with mobilistic common positions and was a major scientific achievement of modern Russian geology, as well as the first universal theory on a global scale, created by Russian geologists.
M.A. Kamaletdinov is author of over 400 scientific papers.
Kamaletdinov was one of the organizers of the Academy of Sciences of Republic of Bashkortostan.
Died on 1 July 2013 in the city of Ufa.

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