Standard

Modeling past and present activity of a subarctic hydrothermal system using O, H, C, U and Th isotopes. / Malov, A.I.; Bolotov, I.N.; Pokrovsky, O.S.; Zykov, S.B.; Tokarev, I.V.; Arslanov, K.; Druzhinin, S.V.; Lyubas, A.A.; Gofarov, M.Y.; Kostikova, I.A.; Kriauciunas, V.V.; Chernov, S.B.; Maksimov, F.E.; Bespalaya, Y.; Aksenova, O.V.

в: Applied Geochemistry, Том 63, 2015, стр. 93-104.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Malov, AI, Bolotov, IN, Pokrovsky, OS, Zykov, SB, Tokarev, IV, Arslanov, K, Druzhinin, SV, Lyubas, AA, Gofarov, MY, Kostikova, IA, Kriauciunas, VV, Chernov, SB, Maksimov, FE, Bespalaya, Y & Aksenova, OV 2015, 'Modeling past and present activity of a subarctic hydrothermal system using O, H, C, U and Th isotopes', Applied Geochemistry, Том. 63, стр. 93-104. https://doi.org/10.1016/j.apgeochem.2015.07.003

APA

Malov, A. I., Bolotov, I. N., Pokrovsky, O. S., Zykov, S. B., Tokarev, I. V., Arslanov, K., Druzhinin, S. V., Lyubas, A. A., Gofarov, M. Y., Kostikova, I. A., Kriauciunas, V. V., Chernov, S. B., Maksimov, F. E., Bespalaya, Y., & Aksenova, O. V. (2015). Modeling past and present activity of a subarctic hydrothermal system using O, H, C, U and Th isotopes. Applied Geochemistry, 63, 93-104. https://doi.org/10.1016/j.apgeochem.2015.07.003

Vancouver

Malov AI, Bolotov IN, Pokrovsky OS, Zykov SB, Tokarev IV, Arslanov K и пр. Modeling past and present activity of a subarctic hydrothermal system using O, H, C, U and Th isotopes. Applied Geochemistry. 2015;63:93-104. https://doi.org/10.1016/j.apgeochem.2015.07.003

Author

Malov, A.I. ; Bolotov, I.N. ; Pokrovsky, O.S. ; Zykov, S.B. ; Tokarev, I.V. ; Arslanov, K. ; Druzhinin, S.V. ; Lyubas, A.A. ; Gofarov, M.Y. ; Kostikova, I.A. ; Kriauciunas, V.V. ; Chernov, S.B. ; Maksimov, F.E. ; Bespalaya, Y. ; Aksenova, O.V. / Modeling past and present activity of a subarctic hydrothermal system using O, H, C, U and Th isotopes. в: Applied Geochemistry. 2015 ; Том 63. стр. 93-104.

BibTeX

@article{09503b58b8e64028b6546f9ecb7d8f66,
title = "Modeling past and present activity of a subarctic hydrothermal system using O, H, C, U and Th isotopes",
abstract = "{\textcopyright} 2015 Elsevier Ltd. The hot springs of the Pymvashor subarctic hydrothermal system are of considerable interest because the area is devoid of recent volcanism and is located in the permafrost region. We attempted to evaluate the activity of thermal waters with respect to host rocks to quantify the water residence time in this system and date the associated travertine. Therefore, we used the chemical composition of the thermal waters, thermodynamic modeling, δ18O and δ2H labels and isotopes, such as 14C-δ13C, 234U-238U, and 230Th-232Th. The δ18O and δ2H values indicated the infiltration of atmospheric water in the recharge area of the hydrothermal system and suggested a stable paleoclimate in the area over the last 5-7.9 thousand years. The fresh water flows through deep parts of the aquifer system where it mixes with brine followed by discharge. The hot springs geothermal water total dissolved solid",
author = "A.I. Malov and I.N. Bolotov and O.S. Pokrovsky and S.B. Zykov and I.V. Tokarev and K. Arslanov and S.V. Druzhinin and A.A. Lyubas and M.Y. Gofarov and I.A. Kostikova and V.V. Kriauciunas and S.B. Chernov and F.E. Maksimov and Y. Bespalaya and O.V. Aksenova",
year = "2015",
doi = "10.1016/j.apgeochem.2015.07.003",
language = "English",
volume = "63",
pages = "93--104",
journal = "Applied Geochemistry",
issn = "0883-2927",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Modeling past and present activity of a subarctic hydrothermal system using O, H, C, U and Th isotopes

AU - Malov, A.I.

AU - Bolotov, I.N.

AU - Pokrovsky, O.S.

AU - Zykov, S.B.

AU - Tokarev, I.V.

AU - Arslanov, K.

AU - Druzhinin, S.V.

AU - Lyubas, A.A.

AU - Gofarov, M.Y.

AU - Kostikova, I.A.

AU - Kriauciunas, V.V.

AU - Chernov, S.B.

AU - Maksimov, F.E.

AU - Bespalaya, Y.

AU - Aksenova, O.V.

PY - 2015

Y1 - 2015

N2 - © 2015 Elsevier Ltd. The hot springs of the Pymvashor subarctic hydrothermal system are of considerable interest because the area is devoid of recent volcanism and is located in the permafrost region. We attempted to evaluate the activity of thermal waters with respect to host rocks to quantify the water residence time in this system and date the associated travertine. Therefore, we used the chemical composition of the thermal waters, thermodynamic modeling, δ18O and δ2H labels and isotopes, such as 14C-δ13C, 234U-238U, and 230Th-232Th. The δ18O and δ2H values indicated the infiltration of atmospheric water in the recharge area of the hydrothermal system and suggested a stable paleoclimate in the area over the last 5-7.9 thousand years. The fresh water flows through deep parts of the aquifer system where it mixes with brine followed by discharge. The hot springs geothermal water total dissolved solid

AB - © 2015 Elsevier Ltd. The hot springs of the Pymvashor subarctic hydrothermal system are of considerable interest because the area is devoid of recent volcanism and is located in the permafrost region. We attempted to evaluate the activity of thermal waters with respect to host rocks to quantify the water residence time in this system and date the associated travertine. Therefore, we used the chemical composition of the thermal waters, thermodynamic modeling, δ18O and δ2H labels and isotopes, such as 14C-δ13C, 234U-238U, and 230Th-232Th. The δ18O and δ2H values indicated the infiltration of atmospheric water in the recharge area of the hydrothermal system and suggested a stable paleoclimate in the area over the last 5-7.9 thousand years. The fresh water flows through deep parts of the aquifer system where it mixes with brine followed by discharge. The hot springs geothermal water total dissolved solid

U2 - 10.1016/j.apgeochem.2015.07.003

DO - 10.1016/j.apgeochem.2015.07.003

M3 - Article

VL - 63

SP - 93

EP - 104

JO - Applied Geochemistry

JF - Applied Geochemistry

SN - 0883-2927

ER -

ID: 3989489