Hydrogeochemistry of processes of dawsonite formation

S. L. Shvartsev

Результат исследований: Материалы для журналаСтатья

2 Цитирования (Scopus)

Выдержка

Considered is the role of dawsonite in underground water-rock system, in which water continuously dissolves endogenous minerals with parallel formation of secondary, sedimentary minerals thus leading to deep differentiation of chemical elements. Investigations were conducted within Berezovoyarskoe dawsonite mineralization located in Tomi basin. The data on dawsonite and other minerals' equilibrium with the sampled underground waters of different geochemical types show that dawsonite, as well as calcite or other secondary minerals, is a product of the water-rock system evolution and is formed at strictly particular stage of this system development, coinciding with the beginning of soda-formation process. Initiation of this stage is possible only after start of calcite precipitation, as it's calcite with whom dawsonite forms paragenetic bonds.

Язык оригиналаАнглийский
Страницы (с-по)818-821
Число страниц4
ЖурналDoklady Akademii Nauk
Том394
Номер выпуска6
СостояниеОпубликовано - 27 окт 2004

Отпечаток

dawsonite
hydrogeochemistry
calcite
mineral
water
chemical element
secondary mineral
rock
mineralization
basin

ASJC Scopus subject areas

  • General

Цитировать

Hydrogeochemistry of processes of dawsonite formation. / Shvartsev, S. L.

В: Doklady Akademii Nauk, Том 394, № 6, 27.10.2004, стр. 818-821.

Результат исследований: Материалы для журналаСтатья

Shvartsev, SL 2004, 'Hydrogeochemistry of processes of dawsonite formation', Doklady Akademii Nauk, том. 394, № 6, стр. 818-821.
Shvartsev, S. L. / Hydrogeochemistry of processes of dawsonite formation. В: Doklady Akademii Nauk. 2004 ; Том 394, № 6. стр. 818-821.
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