ALKALINE WATERS OF THE ULTRABASIC MASSIF OF Mt SOLDATSKAYA, KAMCHATKA: CHEMICAL AND ISOTOPIC COMPOSITION, MINERALOGY AND  14 C AGE OF TRAVERTINES

Yu. A. Taran; Таран Ю. А.; D. P. Savelyev; Савельев Д. П.; G. A. Palyanova; Пальянова Г. А.; B. G. Pokrovsky; Покровский Б. Г.

doi:10.31857/S2686739722602897

ALKALINE WATERS OF THE ULTRABASIC MASSIF OF Mt SOLDATSKAYA, KAMCHATKA: CHEMICAL AND ISOTOPIC COMPOSITION, MINERALOGY AND ¹⁴C AGE OF TRAVERTINES

Авторлар: Taran Y.A.¹, Savelyev D.P.¹, Palyanova G.A.², Pokrovsky B.G.³
Мекемелер:
1. Institute of Volcanology and Seismology, Far Eastern Branch, Russian Academy of Sciences
2. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
3. Geological Institute, Russian Academy of Sciences
Шығарылым: Том 510, № 1 (2023)
Беттер: 30-37
Бөлім: GEOCHEMISTRY
##submission.dateSubmitted##: 14.10.2023
##submission.datePublished##: 01.05.2023
URL: https://bakhtiniada.ru/2686-7397/article/view/135836
DOI: https://doi.org/10.31857/S2686739722602897
EDN: https://elibrary.ru/FFTATX
ID: 135836

Дәйексөз келтіру

Толық мәтін

Ашық рұқсат
Рұқсат жабық

Рұқсат берілді
Рұқсат жабық

Тек жазылушылар үшін

Аннотация
Авторлар туралы
Әдебиет тізімі
Қосымша файлдар
Статистика

Аннотация

For the first time, a detailed description of springs with alkaline waters (pH > 10) found within the ultrabasic massif of the Mt. Soldatskaya on the Kamchatsky Mys Peninsula in Kamchatka is presented. The chemical composition of the springs and the dependence of the ratios and concentrations of some components on pH correspond to the formation of these waters due to modern serpentinization of ultramafic rocks. The most alkaline springs (pH 12.3) contain dissolved hydrogen at a concentration of about 0.6 mmol/l. The behavior of the isotopic composition of carbonate travertines precipitated from these springs (δ¹³C and δ¹⁸O) differs from the known trend for “meteogenic” travertines, associated with serpentinization of ultrabasic rocks in Oman and California. The age of travertines, determined by the radiocarbon method is close to the modern.

Негізгі сөздер

alkaline waters, Kamchatsky Mys Peninsula, ultramafic rocks, serpentinization, age of travertines

Әдебиет тізімі

Barnes I., Lamarche V., JR., Himmelberg G. Geochemical evidence of present-day serpentinization // Science. 1967. V. 156. P. 830–832.
Chavagnac V., Monnin C., Ceuleneer G., Boulart C., Hoareau G. Characterization of hyperalkaline fluids produced by low-temperature serpentinization of mantle peridotites in the Oman and Ligurian ophiolites // Geochemistry, Geophysics and Geosystems. 2013. V. 14 (7). P. 2496–2522.
Dubinina E., Chernyshew I., Bortnikov N., Lein A., Sagalevich A., Gol’zman Y., Bairova E., Mokhov A. Isotopic–geochemical characteristics of the Lost City hydrothermal field // Geochemistry Int. 2007. 45. P. 1131–1143.
Paukert A.N., Matter J.M., Kelemen P.B., Shock E.L., Havig J.R. Reaction path modeling of enhanced in situ CO2 mineralization for carbon sequestration in the peridotite of the Samail Ophiolite, Sultanate of Oman // Chemical Geology. 2012. V. 330. P. 86–100.
Palandri J.L., Reed M.H. Geochemical models of metasomatism in ultramafic systems: Serpentinization, rodingitization, and sea floor carbonate chimney precipitation // Geochimica et Cosmochimica Acta. 2004. V. 68 (5). P. 1115–1133.
Pentecost A. Travertine. Berlin, Springer-Verlag. 2005. 445 p.
Christensen J.N., Watkins J.M., Devriendt L.S., DePao-lo D.J., Conrad M.E., Voltolini M., Yang W., Dong W. Isotopic fractionation accompanying CO2 hydroxylation and carbonate precipitation from high pH waters at The Cedars, California, USA // Geochimica et Cosmochimica Acta. 2021. V. 301. P. 91–115.
Schwarzenbach E.M., Lang S.O., Fruh-Green G.L., Lilley M., Bernasconi S.M., Mehay S. Sources and cycling of carbon in continental, serpentinite-hosted alkaline springs in the Voltri Massif, Italy // Lithos. 2012. V. 177. P. 226–244.
Ternieten L., Früh-Green G.L., Bernasconi S.M. Carbon geochemistry of the active serpentinization site at the Wadi Tayin Massif: Insights from the ICDP Oman Drilling Project: Phase II // Journal of Geophysical Research: Solid Earth. 2021. V. 126. e2021JB022712. https://doi.org/10.1029/2021JB0227
Szponar N., Brazelton W.J., Schrenk M.O., Bower D.M., Steele A., Morrill P.L. Geochemistry of a continental site of serpentinization, the Tablelands Ophiolite, Gros Morne National Park: A Mars analogue // Icarus. 2012. V. 224(2). P. 286–296. https://doi.org/10.1016/j.icarus.2012.07.004
Крайнов С.Р., Рыженко Б.Н., Швец В.М. Геохимия подземных вод. Теоретические, прикладные и экологические аспекты. Москва: Наука, 2004. 677 с.
Савельев Д.П., Новаков Р.М., Черкашин Р.И. Травертины и спелеотемы п-ова Камчатский Мыс (Камчатка) // Вестник КРАУНЦ. Науки о Земле. 2014. № 2 (Выпуск 24). С. 7–11.
Новаков Р.М., Савельев Д.П., Белова Т.П., Пала-марь С.В. Травертины Камчатского Мыса // Материалы конференции, посвященной Дню вулканолога “Вулканизм и связанные с ним процессы”. Петропавловск-Камчатский, ИВиС ДВО РАН. 2014. С. 97–103.
Хотин М.Ю., Шапиро М.Н. Офиолиты Камчатского Мыса (Восточная Камчатка): строение, состав, геодинамические условия формирования // Геотектоника. 2006. № 4. С. 61–89.
Бояринова М.Е., Вешняков Н.А., Коркин А.Г., Савельев Д.П. Государственная геологическая карта Российской Федерации масштаба 1: 200 000. Изд. 2-е. Серия Восточно-Камчатская. Лист 0-58-XXVI, XXXI, XXXII (Усть-Камчатск). Объяснительная записка. СПб.: Картографическая фабрика ВСЕГЕИ, 2007. 226 с. + 2 вкладки.
Reimer P.J., Brown T.A., Reimer Ron W. Discussion: Reporting and calibration of post-bomb 14C data // Radiocarbon. 2004. V. 46 (1). P. 1111–1150.
Reed M.H., Spycher N.F. Calculation of pH and mineral equilibria in hydrothermal waters with application to geothermometry and studies of boiling and dilution // Geochimica et Cosmochimica Acta. 1984. V. 48. P. 1479–1492.
Чешко А.Л., Есиков А.Д. Дейтерий и кислород-18 в атмосферных осадках, поверхностных и грунтовых водах Камчатки и Курильских островов. Водные ресурсы. 1990. № 6. С. 34–43.
Jones B. Review of calcium carbonate polymorph precipitation in spring systems // Sedimentary Geology. 2017. V. 353. P. 64–75.
Horita J. Oxygen and carbon isotope fractionation in the system dolomite–water–CO2 to elevated temperatures // Geochimica et Cosmochimica Acta. 2014. V. 129. P. 111–124.