oilfield-water-analysis_fig1.png|{{figure number|1}}Triangular plot showing relative amounts of cations in typical oil field brines. Relative amount of sodium changes, but calcium is always about five times magnesium. (After Dickey.<ref name=pt05r46>Dickey, P. A., 1966, [http://archives.datapages.com/data/bulletns/1965-67/data/pg/0050/0011/2450/2472.htm Patterns of chemical composition of deep subsurface waters: AAPG Bulletin, v. ]50, p. 2472–2478.</ref>) | oilfield-water-analysis_fig1.png|{{figure number|1}}Triangular plot showing relative amounts of cations in typical oil field brines. Relative amount of sodium changes, but calcium is always about five times magnesium. (After Dickey.<ref name=pt05r46>Dickey, P. A., 1966, [http://archives.datapages.com/data/bulletns/1965-67/data/pg/0050/0011/2450/2472.htm Patterns of chemical composition of deep subsurface waters: AAPG Bulletin, v. ]50, p. 2472–2478.</ref>) |