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Nikolai Kudryavtsev : ウィキペディア英語版
Nikolai Kudryavtsev

Nikolai Alexandrovich Kudryavtsev (ロシア語:Николай Александрович Кудрявцев) (Opochka, October 21, 1893 - Leningrad, December 12, 1971) was a Soviet Russian petroleum geologist. He is the founding father of modern abiogenic theory for origin of petroleum, which states that petroleum is formed from non-biological sources of hydrocarbons located deep in the Earth's crust and mantle.
He graduated from Leningrad Mining Institute in 1922, obtained a Dr.Sc. in Geology and Mineralogy in 1936, and become professor in 1941. Kudryavtsev started his geological career in 1920 at the USSR Geological Committee. In 1929-1971 he worked for All-Union Geological Research Institute (VNIGRI). He suffered from political repressions during Joseph Stalin's regime for his unorthodox thinking, spending several years in Gulag camps in the Transpolar European Russia as an "enemy of the people". After that, he was prohibited from living or staying in central cities of USSR. His only son died defending the Brest Fortress in the beginning of Nazi aggression against USSR.
Kudryavtsev conducted regional geological studies that resulted in discoveries of commercial oil and gas in the Grozny district (Chechnya Autonomy), Central Asia, Timan-Pechora, and other regions of the Soviet Union. He led reconnaissance exploration research in Georgia, and compiled the program of key exploration wells in the West Siberia in 1947 that paved the way to the new era of oil and gas production in Russia that started with first gas gusher near Berezovo in 1953.
== Kudryavtsev's Rule ==
In support of his abiotic theory, Kudryavtsev stated in 1973 (Genesis of Gas and Oil) that any region in which hydrocarbons are found at one level will also have hydrocarbons in large or small quantities at all levels down to and into the basement rock. Thus, where oil and gas deposits are found, there will often be coal seams above them. Gas is usually the deepest in the pattern, and can alternate with oil. All petroleum deposits have a capstone, which is generally impermeable to the upward migration of hydrocarbons. This capstone leads to the accumulation of the hydrocarbon.

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