The chemistry of brines from an Alpine thrust system in the Central Pyrenees: An application of fluid inclusion analysis to the study of fluid behaviour in orogenesis
Quartz filled veins and fractures which formed late in the Alpine thrusting of the Central Pyrenees contain inclusions of hypersaline Na-Ca-Cl brines with total dissolved salts of up to 25 wt%. The total salinity is similar in all samples, irrespective of the vein or the wall rocks, but there are la...
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Veröffentlicht in: | Geochimica et cosmochimica acta 1991-04, Vol.55 (4), p.1021-1030 |
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