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Ultralight Oxygen in Corundum-Bearing Rocks of North Karelia, Russia, as a Result of Isotope Separation by Thermal Diffusion (Soret Effect) in Endogenous Fluid Flow. / Akimova, E. Yu.; Lokhov, K. I.

In: Journal of Materials Science and Chemical Engineering, Vol. 3, No. 3, 2015, p. 42-47.

Research output: Contribution to journal › Article › peer-review

Harvard

Akimova, EY & Lokhov, KI 2015, 'Ultralight Oxygen in Corundum-Bearing Rocks of North Karelia, Russia, as a Result of Isotope Separation by Thermal Diffusion (Soret Effect) in Endogenous Fluid Flow', Journal of Materials Science and Chemical Engineering, vol. 3, no. 3, pp. 42-47. https://doi.org/10.4236/msce.2015.312008

APA

Akimova, E. Y., & Lokhov, K. I. (2015). Ultralight Oxygen in Corundum-Bearing Rocks of North Karelia, Russia, as a Result of Isotope Separation by Thermal Diffusion (Soret Effect) in Endogenous Fluid Flow. Journal of Materials Science and Chemical Engineering, 3(3), 42-47. https://doi.org/10.4236/msce.2015.312008

Vancouver

Akimova EY, Lokhov KI. Ultralight Oxygen in Corundum-Bearing Rocks of North Karelia, Russia, as a Result of Isotope Separation by Thermal Diffusion (Soret Effect) in Endogenous Fluid Flow. Journal of Materials Science and Chemical Engineering. 2015;3(3):42-47. https://doi.org/10.4236/msce.2015.312008

Author

Akimova, E. Yu. ; Lokhov, K. I. / Ultralight Oxygen in Corundum-Bearing Rocks of North Karelia, Russia, as a Result of Isotope Separation by Thermal Diffusion (Soret Effect) in Endogenous Fluid Flow. In: Journal of Materials Science and Chemical Engineering. 2015 ; Vol. 3, No. 3. pp. 42-47.

BibTeX

@article{6c00fc0770c04b599c75d6a721d1e0fe,
title = "Ultralight Oxygen in Corundum-Bearing Rocks of North Karelia, Russia, as a Result of Isotope Separation by Thermal Diffusion (Soret Effect) in Endogenous Fluid Flow",
abstract = "Helium and argon isotopes in fluid inclusions in minerals of corundum bearing rocks with anomalous light oxygen of the Khitoostrov (North Karelia, Russia) were studied. It was found that atmospheric noble gas component is missing. Therefore, all previously proposed models of participation in the fluid surface ice meltwater are not valid. Proposed and justified endogenous mechanism of isotope fractionation of oxygen and other chemical elements by the mechanism of thermal diffusion. Geologically justified existence of the cascading effect for a number of the separation thermodiffusion cells, which lead to significant isotope effects. Cascading is realized due to the “fluid pump”, in which role are acting amphibolized gabbro in the contact with corundum metasomatites. It is assumed that the mechanism is not specific for the case corundum metasomatic rocks, which are a special case of manifestation of such a scenario in processes involving endogenous fluid flows.",
keywords = "Corundum-Bearing Rocks, Noble Gas Isotopes, Anomaliously Light Oxygen, Thermodiffusion, Natural Fluid Pump",
author = "Akimova, {E. Yu.} and Lokhov, {K. I.}",
year = "2015",
doi = "10.4236/msce.2015.312008",
language = "English",
volume = "3",
pages = "42--47",
journal = "Journal of Materials Science and Chemical Engineering",
issn = "2327-6045",
publisher = "Scientific Research",
number = "3",

}

RIS

TY - JOUR

T1 - Ultralight Oxygen in Corundum-Bearing Rocks of North Karelia, Russia, as a Result of Isotope Separation by Thermal Diffusion (Soret Effect) in Endogenous Fluid Flow

AU - Akimova, E. Yu.

AU - Lokhov, K. I.

PY - 2015

Y1 - 2015

N2 - Helium and argon isotopes in fluid inclusions in minerals of corundum bearing rocks with anomalous light oxygen of the Khitoostrov (North Karelia, Russia) were studied. It was found that atmospheric noble gas component is missing. Therefore, all previously proposed models of participation in the fluid surface ice meltwater are not valid. Proposed and justified endogenous mechanism of isotope fractionation of oxygen and other chemical elements by the mechanism of thermal diffusion. Geologically justified existence of the cascading effect for a number of the separation thermodiffusion cells, which lead to significant isotope effects. Cascading is realized due to the “fluid pump”, in which role are acting amphibolized gabbro in the contact with corundum metasomatites. It is assumed that the mechanism is not specific for the case corundum metasomatic rocks, which are a special case of manifestation of such a scenario in processes involving endogenous fluid flows.

AB - Helium and argon isotopes in fluid inclusions in minerals of corundum bearing rocks with anomalous light oxygen of the Khitoostrov (North Karelia, Russia) were studied. It was found that atmospheric noble gas component is missing. Therefore, all previously proposed models of participation in the fluid surface ice meltwater are not valid. Proposed and justified endogenous mechanism of isotope fractionation of oxygen and other chemical elements by the mechanism of thermal diffusion. Geologically justified existence of the cascading effect for a number of the separation thermodiffusion cells, which lead to significant isotope effects. Cascading is realized due to the “fluid pump”, in which role are acting amphibolized gabbro in the contact with corundum metasomatites. It is assumed that the mechanism is not specific for the case corundum metasomatic rocks, which are a special case of manifestation of such a scenario in processes involving endogenous fluid flows.

KW - Corundum-Bearing Rocks

KW - Noble Gas Isotopes

KW - Anomaliously Light Oxygen

KW - Thermodiffusion

KW - Natural Fluid Pump

U2 - 10.4236/msce.2015.312008

DO - 10.4236/msce.2015.312008

M3 - Article

VL - 3

SP - 42

EP - 47

JO - Journal of Materials Science and Chemical Engineering

JF - Journal of Materials Science and Chemical Engineering

SN - 2327-6045

IS - 3

ER -

ID: 5818040