Lead distribution in coal and coaly shales in the Upper Silesian Coal Basin

Authors

  • Henryk Parzentny xxx

Abstract

Lend in the Upper Silesian Coal Basin is mainly of inorganic origin. Its average content, in coal and coaly shales of the paralic series, is higher in the western part of the basin. In the limnic series, it is higher in the eastern part of the basin'. Great differentiation between the quantity of lead of organic and inorganic origin in individual beds in the Upper Silesian Coal Basin has been observed. A great contrast between the influence of organic and inorganic matter on the average content of this element has been ascertained. It testifies the great dynamics of lead accumulation and dispersion. Differences of lead content in the beds are correlated to the distribution of maximal extensive accumulation and dispersion of lead.

Downloads

Published

2013-03-03

Issue

Vol. 38 No. 1 (1994)

Section

Articles

License

Authors who publish with this journal agree to the following terms:
  1. 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.
  2. 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.
  3. 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).