Neogene lacustrine sediments and authigenic minerals geochemical characteristics

  • Jelena Obradović University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade
  • Nebojša Vasić University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade
  • Milica Kašanin-Grubin University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade
  • Nenad Grubin University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade
Keywords: Neogene, lacustrine sedimentation, authigenic minerals, geochemical caracteristics

Abstract

During Neogene, especially from Oligocene to Pliocene, many lacustrine basins were developed on the territory of Serbia due to activity of several tectonic cycles that generally were controlled by formation and evolution of the Pannonian basin. This paper concerns the occurences of authigenic minerals within sediments of  lacustrine basins, especially silicates, aluminum silicatcs, borosilicates, carbonates, complex boron-phosphate minerals  and sulfides, and their geochemical characteristics.

 

Published
2000-12-20
How to Cite
Obradović, J., Vasić, N., Kašanin-Grubin, M. and Grubin, N. (2000) “Neogene lacustrine sediments and authigenic minerals geochemical characteristics”, Geološki anali Balkanskoga poluostrva, 63(1), pp. 135-154. Available at: https://gabp.rgf.rs/index.php/gabp/article/view/301 (Accessed: 22December2024).
Issue
Vol 63 No 1 (2000): Geološki anali Balkanskoga poluostrva
Section
Original Scientific Paper

Copyright (c) 2000 Geološki anali Balkanskoga poluostrva

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