电邮这篇文章 Uptake of Dissolved Fluorine from Seawater During Halmyrolysis of Igneous Rocks
- 作者: Savenko A.V.1, Savenko V.S.1
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隶属关系:
- Lomonosov Moscow State University
- 期: 卷 522, 编号 2 (2025)
- 页面: 249-252
- 栏目: GEOCHEMISTRY
- ##submission.dateSubmitted##: 15.10.2025
- ##submission.datePublished##: 15.06.2025
- URL: https://rjeid.com/2686-7397/article/view/693299
- DOI: https://doi.org/10.31857/S2686739725060094
- ID: 693299
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详细
According to long-term 6-year experiments, a significant decrease in the concentration of dissolved fluorine in seawater was established during its interaction with ultrabasic and basic igneous rocks: dunite, gabbro-norite, and basalt. It is concluded that submarine weathering (halmyrolysis) of rocks of the oceanic crust is a significant expenditure item in the geochemical balance of fluorine in the World Ocean.
作者简介
A. Savenko
Lomonosov Moscow State University
Email: Alla_Savenko@rambler.ru
Moscow, Russia
V. Savenko
Lomonosov Moscow State UniversityMoscow, Russia
参考
- Rude P.D., Aller R.C. Fluorine mobility during early diagenesis of carbonate sediment: An indicator of mineral transformations // Geochim. et Cosmochim. Acta. 1991. V. 55. № 9. P. 2491–2509.
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- Григорьев Н.А. Среднее содержание химических элементов в горных породах, слагающих верхнюю часть континентальной коры // Геохимия. 2003. № 7. С. 785–792.
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