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Abstract

The evolution of sedimentary basins can be explored by analyzing the changes in their lithologies and lithofacies (i.e. predominant lithologies). The Greater Caucasus Basin, which was located at the northern margin of the Neotethys Ocean, represents a complete Sinemurian-Tithonian succession. A quantitative analysis of compiled datasets suggests that principal lithologies and lithofacies are represented by siliciclastics, shale and carbonates. The relative abundance of siliciclastics and shale decreased throughout the Jurassic, whereas that of carbonates increased. Evaporites are known from the Upper Jurassic, while volcaniclastics and volcanics, as well as coals, are known only in the Lower to Middle Jurassic. Siliceous rocks are extremely rare. Lithology and lithofacies proportions change accordingly. The Sinemurian-Bathonian sedimentary complex is siliciclastic-and-shale-dominated, whereas the Callovian-Tithonian sedimentary complex is carbonate-dominated. A major change in the character of sedimentation occurred during the Aalenian-Callovian time interval. Regional transgressions and regressions were more important controls of changes in the sedimentary rock proportions than average basin depth. Landward shoreline shifts were especially favorable for carbonate accumulation, whereas siliciclastics and shale were deposited preferentially in regressive settings. An extended area of the marine basin, its lower average depth, and a sharp bathymetric gradient favored a higher diversity of sedimentation. An orogeny at the Triassic-Jurassic transition was responsible for a large proportion of siliciclastics and extensive conglomerate deposition. An arcarc collision in the Middle Jurassic also enhanced the siliciclastic deposition. Both phases of tectonic activity were linked with an increase in volcanics and volcaniclastics. Volcanism itself might have been an important control on sedimentation. A transition to carbonate-dominated sedimentation occurred in the Late Jurassic, reflecting a tectonically calm period.

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Editor(s)-in-Chief: Demény, Attila

Deputy Editor(s)-in-Chief: Raucsik, Béla

Co-ordinating Editor(s): Schmiedl, Gábor

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  • Dobosi, Gábor (Geochemistry)
  • Haas, János Regional Geology and Sedimentology)
  • Márton, Emő (Geodynamics)
  • Ősi, Attila (paleontology)
  • Seghedy, Ioan (petrology and geochemistry)
  • Zajzon, Norbert (petrology and geochemistry)
  • Németh, Norbert (structural geology)
  • Kövér, Szilvia (sedimentology)
  • Götz, Anette (sedimentology)
  • Mojzsis, Stephen J. (petrology, geochemistry and planetology)
  • Hatvani, István Gábor (geomathematics)
  • Pálfy, József (Fossils and Stratigraphic Records)
  • Pogácsás, György (Petroleum Geology)
  • M. Tóth, Tivadar (Mineralogy, Petrology)
  • Török, Ákos (Applied and Environmental Earth Sciences)
  • Henry M. Lieberman (Language Editor)

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Due to the changes in editorial functions, the Advisory Board has been terminated. The participation of former Advisory Board members is highly appreciated and gratefully thanked.

CENTRAL EUROPEAN GEOLOGY
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Hungarian Academy of Sciences
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