Stable isotope geochemistry and the genesis of the Polish native sulphur deposits - a review
Abstract
The study summarizes earlier data concerning of sulphur, carbon, and oxygen isotope ratios in Polish native sulphur deposits of the Carpathian Foredeep. It characterizes isotope compositions of the Miocene evaporite rocks such as gypsum (the host-rocks for sulphur ores), native sulphur, postgypsum limestones, and residual sulphates (celestite, barite, and aquaeous sulpates of ore water). Based upon available isotopic results the authors have proposed a model for genesis of Polish sulphur ores which includes: origin of ore-forming factors, mechanisms of ore-forming processes, capacity of sulphate-reduction process, origin of the ore water, how open the system was and the problem of sulphur ore disintegration.Downloads
Published
2013-03-02
Issue
Section
Articles
License
Authors who publish with this journal agree to the following terms:- Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
- Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
- Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as this can lead to productive exchanges and earlier and more frequent citation of the published work (See The Effect of Open Access).