Application of brine differentiation and Langelier-Ludwig plots to fresh-to-brine waters from sedimentary basins: Diagnostic potentials and limits

被引:23
作者
Boschetti, Tiziano [1 ]
机构
[1] Univ Parma, Dept Earth Sci, I-43100 Parma, Italy
关键词
Sedimentary basins; Brine waters; Salinization processes; Major dissolved constituents; MUD VOLCANOS; NORTHERN APENNINES; FLUID MIGRATION; ORIGIN; BORON; EVOLUTION; AZERBAIJAN; GAS;
D O I
10.1016/j.gexplo.2010.12.002
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Classical chemical classification plots that use major anions and cations can discern between different water facies but they do not offer sufficient discriminatory power for salt waters from sedimentary basins, whose origin is therefore frequently misunderstood. The Brine Differentiation Plot (BDP) was proposed by Hounslow (1995) in order to investigate the brine genesis, principally evaporite dissolution, alkali lakes and oilfield brines. However, its diagnostic potential has been undervalued so far. In this paper, the potential of BDP was tested and compared with the classical Langelier-Ludwig plot using concentration of major dissolved constituents of fresh to brine waters from different sedimentary basins (Northern Apennine Foredeep, Italy; Provence Basin, Western Mediterranean; Caucasus; Trinidad). Mixing processes between different water types as evaluated by these diagrams would seem to be constrained by the boron-chloride plot. (c) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:126 / 130
页数:5
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