Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Boris G. Polyak"'
Publikováno v:
Frontiers of Earth Science. 14:738-757
The generation temperatures of gas-water fluids released from mud volcanoes in different provinces of the Caucasian region have been constrained using Mg/Li (TMg/Li) chemical geothermometry. Mud volcanic fluids in the Taman Peninsula (Kerch-Taman mud
Publikováno v:
Chemical Geology. 471
Noble gases may be considered as the most prominent tracers of natural fluids, including hydrocarbons. The atmosphere is the only source of 20Ne, 36Ar, 84Kr, 130Xe in subsurface environments, and their concentrations in pore waters after recharge are
Autor:
Igor L. Kamenskii, E. M. Prasolov, Vassilii Yu. Lavrushin, Boris G. Polyak, Andrew L. Cheshko
Publikováno v:
Chemical Geology. 339:127-140
Thermal springs with water temperatures up to 97 °C were sampled in the Chukotka Peninsula of the north-eastern Asia on the area of ~ 60,000 km2. He and Ar isotope ratios in bubbling gases were measured in 30 samples of from 23 spring groups. 3Не/
Publikováno v:
Chemical Geology. 266:57-66
The isotope composition of He contained in gas phase of subsurface fluids in the Greater Caucasus orogene and adjacent areas is revisited combining data obtained before 1998 with 54 new measurements. We report 3He/4He = R ratios (hereafter, R) in CO2
Autor:
Joris M. Gieskes, Annette Deyhle, Guram I. Buachidze, Klaus Wallmann, Anton Eisenhauer, Vasili Yu. Lavrushin, Achim J Kopf, Boris G. Polyak
Publikováno v:
International Journal of Earth Sciences. 92:407-425
The Caucasian orogenic wedge formed as a consequence of the closure of the Tethyan Ocean, and numerous fields of active mud volcanoes pepper the area adjacent to the Black and Caspian Seas. Stable isotope ratios of boron, helium, and carbon have been
Publikováno v:
Geochimica et Cosmochimica Acta. 64:1925-1944
109 new measurements of 3He/4He ≡ R in subsurface fluids of the Northern Caucasus coupled with the data obtained previously allow regional regularities in the distribution of helium isotopic composition to be examined. Cis-Caucasian foredeeps show
Autor:
I. N. Tolstikhin, E. M. Prasolov, Boris G. Polyak, M. D. Khutorskoy, S. V. Kozlovtseva, V. I. Kononov
Publikováno v:
International Geology Review. 35:186-202
The isotopic composition of helium in subterranean fluids from 34 locations in southern Siberia and northern Mongolia has been measured- The ratio 3He/4He ranges from radiogenic (∼10−8) to mantle (∼10−5) values. For the most part, the hydroca
Autor:
Ph. Bouysse, V.I. Paduchikh, Boris G. Polyak, A. Criaud, M. D. Khutorskoy, E.P. Radionova, I. N. Tolstikhin, V. I. Kononov, A.I. Voznesenskiy, A. A. Rot, V. G. Matveev, V.I. Dvorov, V.P. Zverev, G. Yu. Butuzova
Publikováno v:
Journal of Volcanology and Geothermal Research. 54:81-105
During the Soviet-French survey carried out on board of the R.V. Akademik N. Strakhov , between Guadeloupe and Montserrat island in the central Lesser Antilles, evidence of submarine hydrothermal activity was discovered on the southeastern tip of the
Autor:
Boris 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 consid
Autor:
Igor Tolstikhin, Boris G. Polyak
Publikováno v:
Chemical Geology: Isotope Geoscience section. 52:9-33
The isotopic composition of helium ( 3 He 4 He = R ) contained in underground fluids was studied in different geotectonic provinces. Provincial mean values ( R ) were estimated by a routine statistic procedure. The R - values were found to depend on