Zobrazeno 1 - 10
of 29
pro vyhledávání: '"B. G. Polyak"'
Autor:
B. G. Polyak
Publikováno v:
Geofísica Internacional, Vol 41, Iss 4, Pp 485-490 (2002)
Se realizó el estudio de la relación R = (3He/ 4He) en fluidos subterráneos de 104 sitios de la zona Baikal Rift y zonas adyacentes de Rusia y Mongolia. Los valores de la relación varían desde 1 E-8 (que es un valor típico para He radiogénico
Externí odkaz:
https://doaj.org/article/a6165a8e36cf4a749c3f3db92c5939c5
Autor:
B. G. Polyak
Publikováno v:
Annals of Geophysics, Vol 48, Iss 1 (2005)
Terrestrial heat flow density, q, is inversely correlated with the age, t, of tectono-magmatic activity in the Earth's crust (Polyak and Smirnov, 1966; etc.). «Heat flow-age dependence» indicates unknown temporal heat sources in the interior cons
Externí odkaz:
https://doaj.org/article/80ae8a577f10486588dc3e75a730380c
Publikováno v:
Izvestiya, Physics of the Solid Earth. 56:490-510
The geophysical and geochemical indicators of the ascending heat and mass flow in the continental crust—conductive heat flow through the surface of the crust and the isotopic composition of helium in freely circulating underground fluids—are cons
Autor:
B. G. Polyak, B. Deneva, R. Nakov, A. V. Ermakov, O. E. Kikvadze, V. Hristov, I. L. Kamenskii, V. Yu. Lavrushin
Publikováno v:
Lithology and Mineral Resources. 55:131-138
The geothermal and hydrochemical parameters of a large hydrogeothermal system located in the city of Velingrad and its environs (southwestern Bulgaria) are discussed. The article summarizes the results of its research, including those obtained by 201
Publikováno v:
Lithology and Mineral Resources. 53:380-393
The paper presents data on the composition of a gas phase of underground fluids in the East Carpathian region, including 3He/4He, 40Ar/36Ar, and 4He/20Ne ratios. The argon isotope composition of these gases was used to estimate the fractions of atmos
Autor:
B. G. Polyak, Yu. G. Israfailov, V. Yu. Lavrushin, M. I. Bujakaite, I. L. Kamensky, Boris G. Pokrovsky
Publikováno v:
Lithology and Mineral Resources. 53:53-75
It is shown that the gas and water phases of the thermal nitrogen–methane waters in the Talysh fold zone of the Lesser Caucasus mountain system contain helium and strontium with mantle isotope signatures (3Не/4Не from 200 × 10–8 to 401 × 10
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 929:012005
The research shows new results of isotope-helium studies carried out in the Tien Shan - Naryn and Atbashi basins. Sampling of thermal mineral springs in the Eastern Tien Shan was carried out in order to identify traces of mantle emanations in fluids
Autor:
M. D. Khutorskoi, B. G. Polyak
Publikováno v:
Geotectonics. 51:152-162
The paper reports on the morphostructure and heat flow in zones of transform faults of the North Atlantic and the Southeast Pacific, focusing on the fundamental difference between heat flow in active and inactive parts of the faults. In the active pa
Autor:
M. D. Khutorskoi, B. G. Polyak
Publikováno v:
Geotectonics. 50:179-195
Heat generation due to decay of long-lived radioactive isotopes is considered in the Earth’s crust of the Archean–Proterozoic and Paleozoic provinces of Eurasia and North America. The heat flow that forms in the mantle is calculated as the differ
Autor:
M. D. Khutorskoy, B. G. Polyak
Publikováno v:
Геотектоника. :43-61