Geochemistry of the thermal waters of Sikhote Alin

Chudaev, Oleg; Chudaeva, V. A.; Bragin, I.V.

doi:10.1134/s1819714008060079

Cited by 8 publications

(14 citation statements)

References 3 publications

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“…The Annenskiy thermal spring is located in the Khabarovskiy region, Russia, in the lower reaches of the Amur River, on its right bank, 120 km upstream from the town of Nikolaevsk-on-Amur, 6.5 km to the southwest from the Susanino pier [1][2][3] (Fig. 1).…”

Section: Geology and Hydrogeologymentioning

confidence: 99%

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The Annenskiy thermal waters as the certain stage of the water-rock interaction (Far East, Russia)

et al. 2019

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Chemical composition and saturation degree of the Annenskiy thermal waters to minerals of water-bearing rock have been considered in the manuscript. It is shown that the thermal waters are low mineralized, alkaline and belong to HCO3-Na type. The thermal waters-rock system is equilibrium-nonequilibrium. It means that the waters dissolve primary minerals continuously, never reaching saturation (anorthite, K-field spar and etc.), and form new secondary mineral phases simultaneously, reaching saturation (gibbsite, montmorillonite, albite and etc.). Besides, peculiarities of the equilibrium with minerals of water-bearing rocks for surface and ground waters of the studied region was considered. It is established that the thermal waters are ahead of surface and ground waters and represent the certain stage of the water-rock system evolution. The stage is characterized by the certain chemical composition (TDS=148-317 mg/L, HCO3-Na, SiO2=9-80 mg/L), complex of secondary minerals (calcite, albite, laumontite and etc.) and special geochemical environment (pH 8.2-8.6).

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Section: Geology and Hydrogeologymentioning

confidence: 99%

“…It should be noticed that the series of manuscripts are dedicated to the origin of thermal waters of the Far East, Russia [1][2][3]. However, the formation processes of the Annenskiy thermal waters has never been considered before in accordance with the concept of the geological evolution of the water-rock system.…”

Section: Introductionmentioning

confidence: 99%

The Annenskiy thermal waters as the certain stage of the water-rock interaction (Far East, Russia)

et al. 2019

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“…Стоит, несомненно, отменить работы по подземным водам Северо-Востока России [5,6], которые, в основном, имеют гидрологическую и гидрогеологическую направленность. Несмотря на наличие комплексных работ по термам Дальнего Востока [10,15,17,18], термальные воды Магаданской области остались без должного внимания.…”

Section: Introductionunclassified

New Isotope-Geochemical Data on Thermal Waters of the Talskoe Deposit (Magadan Oblast)

Bragin¹,

Челноков²,

Харитонова³

2021

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In this paper, we summarize new data on the chemical and isotopic composition of thermal wa-ters of the Talskoye deposit in the Magadan Oblast. We were the first to obtain the data on the content of stable oxygen (δ18O) and hydrogen (δD) isotopes in thermal and background waters, as well as oxygen (δ18O) and carbon in bicarbonate ion (δ13C), even though this is the largest ex-ploited deposit of low-mineralized alkaline nitric thermal waters in the region. The thermal water is fresh (M = 980 mg/l), alkaline (pH = 8.9), hydrocarbonate-chloride-sulphate sodium with a high content of fluorine (up to 17 mg/l) and silicic acid (up to 152 mg/l). The deposit is fed by atmospheric precipitation; we did not find traces of melting underground ice supply. A sequential scheme for calculating the temperature of a deep reservoir was applied, which allowed the temperature of water formation to be constrained at 108 °C suggesting an input of fluids rich in potassium and sulfate ion.

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“…ВВЕДЕНИЕ Проявления термальных вод, расположенных на побережье континентальной части Дальнего Востока России, привлекают большое внимание широкого круга специалистов [2][3][4][5][6][7][8][9][10][11], однако, из-за отдаленности и недоступности, остаются плохо изученными. Основной целью данной работы было изучение условий формирования и генезиса термальных вод побережья Охотского моря Хабаровского края и Магаданской области и сравнение дан-ных с ранее изученными районами Сахалина и Камчатки.…”

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“…Методика исследований является стандартной и подробно описана в работах [8,9]. РЕЗУЛЬТАТЫ И ОБСУЖДЕНИЕ В зависимости от гидрогеологических условий воды формируют свой состав либо в кристаллических, либо в осадочных породах [9,10,11]. Границы этих резервуаров разрушаются неотектоникой, а источником тепла считаются молодые интрузии.…”

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Features of Rare-Earth Elements Behavior and the Conditions of Water Recharge of the Thermal Waters of the Sea of Okhotsk Sea Shore

Bragin¹,

Veldemar²,

Pavlov³

et al. 2020

Water-Rock Interaction: Geological Evolution

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В статье представлены новые данные по геохимии редкоземельных элементов, а также изотопии термальных вод Охотоморского побережья (Ульский, Анненский, Тумнин, Таватум, Талая, Паратунка, Даги и Лесогорский). Для изученной группы термальных определены основные геолого-гидрогеологические условия формирования их состава. Профили распределения редкоземельных элементов (РЗЭ) позволило разделить исследованную группу термальных вод по водовмещающим породам, минерализации и окислительновосстановительным условиям областей разгрузки вод. Значения δ18O и δD позволило выделить основные факторы, определяющие особенности питания вод: климат, географическое положение, особенности гидрологии в высоких широтах.

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Geochemistry of the thermal waters of Sikhote Alin

Cited by 8 publications

References 3 publications

The Annenskiy thermal waters as the certain stage of the water-rock interaction (Far East, Russia)

The Annenskiy thermal waters as the certain stage of the water-rock interaction (Far East, Russia)

New Isotope-Geochemical Data on Thermal Waters of the Talskoe Deposit (Magadan Oblast)

Features of Rare-Earth Elements Behavior and the Conditions of Water Recharge of the Thermal Waters of the Sea of Okhotsk Sea Shore

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