GEOLOGICA BALCANICA, 33. 3-4, Sofia, Decemb. 2003, p. 15-22 Palaeogene sediments (Mechit Formation) near Panagyurishte and Strelcha (Sredna gora Mts.) Ivan Boyanov, Ivan Zagorchev, Aleksander Goranov Geological Institute, Bulgarian Academy of Sciences. 1113 Sofia; E-mail
[email protected] (submitted: 1. 12. 2203; accepted for publication: 22. 12. 2003) H6. DOJ/H06, H6. 3azop'le6, AA. ropaH06. - flaAeozeHo- Abstract. The newly-introduced Mechit Formation is a 6ble ocaoo'lHbte nopoobl (Me'lumcKaJ/ cGuma) 6 pauoHe continental (fluvial) sequence of conglomerates and flaHa210puwme u CmpeA'lU (CpeoHozopue). HosoycTa sandstones with occasional clays and coalefied plant de HOBJieHHall Me\fHTCKall CBHTa CJio:>KeHa KOHTHHeHTaJib bris. The pebbles derived from pre-Alpine basement HOH llOCJieJ].OBaTeJibHOCTbiO - pe'IHbiMH KOHrJIOMepa rocks (gneisses, amphibolites, granites, pegmatites) and TaMH H neC\faHHKaMH, MeCTaMH - C rJIHHHCTbiMH npOCJIO Upper Cretaceous (Coniacian - Campanian) sedimen liMH H o6yrneHHbiMH pacTHTeJibHbiMH o6noMKaMH. B tary, volcanic and intrusive rocks and ores. The forma raJi bKax npe.ncTasneHbi nopOJJ.bi .noaJibnHikKoro ocHosa tion is more than 570 m thick. It covers with unconform HHll (rHeHCbl, aM<flH60JIHTbl, rpaHHTbl H nerMaTHTbl) H able depositional contact Maastrichtian flysch and older sepxHeMeJIOBbie (KOHbliK-KaMnaHCKHe) oca.no'IHbie, syn Cretaceous and pre-Cretaceous rocks, and forms denu KaHH'IeCKHe H llJIYTOHH\feCKHe nopO.Il.bl, a TaK)I(e - opy dation pockets and neptunian clastic dykes in the pre .neHeHHll. MowHOCTb Me'IHTCKOH CBHTbi 6onee 570 m. Cretaceous basement. On the basis of taxa from the 0Ha 3aJieraeT HeCOrJiaCHO Ha MaacTpHXTCKOM <flJIHWe H Normapolles group, the formation is referred to upper Ha 6onee .npeBHHX MeJIOBbiX H .noMeJIOBbiX nopo.nax.