Article ID Journal Published Year Pages File Type
4702092 Geochimica et Cosmochimica Acta 2014 4 Pages PDF
Abstract

Recently Steele-MacInnis and Bodnar reported an experimental study on the estimation of the salinity of halite bearing fluid inclusions from dissolution temperatures of halite crystals, in the presence and absence of a vapour phase Steele-MacInnis and Bodnar (2013). The authors present new purely empirical equations to calculate fluid inclusion bulk salinity, which is mainly determined by dissolution temperature of halite (SLV→LV) with a minor correction due to presence of a vapour phase at higher temperatures, similar to the study of Bakker (2012). The experimental approach in their work is inappropriate, it does not provide experimental data, and it does not illustrate an estimate of uncertainty, accuracy and precision of the results. The mathematical modelling with purely empirical best-fit equations is insufficient, and partly erroneous. Comparison with the model from Bakker (2012) results in highly incorrect, inconsistent and imprecise statements about the quality of the results from Bakker (2012). Furthermore, the authors use “supplementary data” to continue a discussion without peer-review.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
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