Hydrogeochemical and isotopic signatures elucidate deep subsurface hypersaline brine formation through radiolysis driven water-rock interaction

Author:

Nisson D.M.,Kieft T.L.,Drake H.,Warr O.,Sherwood Lollar B.,Ogasawara H.,Perl S.M.,Friefeld B.M.,Castillo J.,Whitehouse M.J.,Kooijman E.,Onstott T.C.

Funder

National Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference149 articles.

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4. Radiolytic products in waters;Bjergbakke;Radiochim. Acta.,1989

5. Blomqvist, R., 1999. Hydrogeochemistry of deep groundwaters in the central part of the Fennoscandian Shield. In: Geological Survey of Finland, Nuclear Waste Disposal Research, Report (No. GTK-YST-101). pp. 3–37.

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