Figure 2. Correlation of Late Paleozoic tectonic events in the Pripyat Trough and those in the
adjacent basins of the western part of the Sarmatian-Turanian lineament and Lvov-Lyublin marginal trough
[Aisberg et al., 2004].
(I) geologic events, (II) rock formations, (III) maximum thickness of the rocks. Sedimentary rocks:
(1) carbonate rocks, (2) argillaceous-carbonate and carbonate-argillaceous rocks, (3) argillaceous rocks,
(4) siliceous-carbonate rocks, (5) terrigenous-carbonate and carbonate-terrigenous rocks, (6) argillaceous-arenaceous-carbonate
and argillaceous-carbonate-arenaceous, rocks, (7) terrigenous-sulfate-carbonate and sulfate-carbonate terrigenous rocks,
(8) sulfate-carbonate-argillaceous and argillaceous-sulfate-carbonate rocks, (9) arenaceous-argillaceous rocks,
(10) arenaceous rocks, (11) terrigenous rocks, (12) terrigenous-flyschoid rocks, (13) terrigenous molassic
rocks, (14) paralic coal-bearing carbonate-terrigenous rocks, (15) terrigenous coal-bearing paralic rocks,
(16) coal- and bauxite-bearing quartz-kaolinized rocks, (17) salt-bearing (halogenized) rocks, (18) salt-bearing
terrigenous and mixed sedimentary-volcanic rocks, (19) volcanic-carbonate rocks, (20) tuffaceous
clay-sulfate-carbonate rocks, (21) igneous (volcanic) rocks: (22) alkaline ultrabasic to alkaline basaltic
rocks: (23) basalt, (24) andesite, (25) trachybasalt-trachyandesite-trachyrhyolite, (26) unconformity;
(27) break in sedimentation.