BELA PALAIKA

More documents

Recommendations

Info

Urosevic D. (1968): RAZVICE TRIJASKIH I JURSKIH SEDIMENATA NA ZAPADNOM KRILU KU RILOVSKE ANTIKLINALE. Vesnik Zavoda za geol. i geof. istraz., A, 26, Beograd. Veselinovic D. (1967): KRATAK PRIKAZ GEOLOGI]E NEKIH LOKALNOSTI Du2 PUTA PIROT -BABUSNICA-BELA PALANKA-SICEVACKA KLISURA-NISKA BANJA. 8. kongres KBGA, Vodic za ekskurziju, Beograd. Veselinovic M. (1959): PRETHODNO SAOPSTENJE 0 NALASKU STARIJEG PALEOZOIKA NA SUVOJ PLANINI. Zapisnici SGD za 1957. godinu, Beograd. Veselinovic M. (1962): STARIJE PALEOZOJSKE TVOREVINE NA SUVOJ PLANINI I PARALELI ZACIJA ISTIH SA SUSEDNIM OBLASTIMA U ISTOCNOJ SRBIJI. Zapisnici SGD za 1958. i 1959. godinu, Beograd. Veselinovic M. (1964): STARIJI PALEOZOIK ISTOCNE SRBlJE - FACIJE I PARALELE (DOKTOR SKA DISERTACIJA). Geol. anaH Balk. Pol., 31, Beograd. Viquesnel A. (1842): JOURNAL D'UN VOYAGE DANS LA TORQUIE D'EUROPE. Mem. de la Soc. geol. de France, 5, Paris. 2ujovic J. (1884): GRADA ZA GEOLOGIJU KRALJEVINE SRBIJE. PRILOG ZA GEOLOGIJU JU GOISTOCNE SRBIJE. Beograd. 2ujovic J. (1893): GEOLOGIJA SRBI]E, IDEO. Posebno izdanje SKA, 4,/Beograd. 63
GEOLOGY OF THE SHEET BELA P ALANKA THE SHEET BELA PALANKA HAS BEEN MAPPED AND THE EXPLANATORY TEXT PREPARED BY THE STAFF OF THE INSTITUTE FOR GEOLOGICAL AND GEOPHYSICAL RESEARCH, BELGRADE. The oldest rocks in the sheet-covered area are Upper Proterozoic, Proterozoic-Cambrian and Cambrian crystalline schists of Selicevica, Babicka Gora and Krusevica, green schist facies. These oldest rocks are geosynclinal, predominantly sedimentary formations: albitic-chloritic-muscovitic schist with lenses of albitic, actinolitic and chloritic-epidote schists and muscovitic quartzite. In the late Proterozoic and early Cambrian, volcanogenic-sedimentary rocks are formed (now mostly muscovitic-albitic-chloritic-quartz schist with concordant bodies or metamorphosed alkaline and acid magmatic rocks). These are covered with Cambrian quartz conglomerate and quartzite, followed by sericitic-chloritic and quartz schists with some metamorphosed alkaline and acid magmatic rocks. Other Palaeozoic formations are recognized in the east of the sheet. The Upper Silurian consists of limestone with orthocerases and crinoids of the core of Stara Planina anticline. Schist and metasandstone of Modra Stena which contains gabbro and diabase sills are also supposed to be of the Silurian. The Lower Devonian is substantiated by fauna, and the Middle and Upper Devonian age of flysch is documented by floral remains. Carboniferous fOlmations consists of conglomerate, sandstone and shale, which lie unconformably over the Devonian and pass upward into PeImian red sandstone. Plagiogranite, which penetrates Silurian sediments in the core of Stara Planina anticline, is probably also of the Carboniferous. Mesozoic fOlmations are most widespread in the sheet. Lower Triassic sediments are transgressive over red sandstone and consist of Seissian coarse clastics and Campilian limestone, dolomite and arkose with lamelibranchs. The Middle Jurassic is composed of thin transgressive calcareous and clastic rocks. These gradually develop into neritic dolomitic limestone of the Oxfordian and Kimmeridgian and pass into reef and subreef limestone of the Tithonian. The Tithonian also contains flysch with large olistoliths of Jurassic reef limestone. Lower Cretaceous sediments are the most widely spread Mesozoic fonnations which develop conformably from Jurassic. These are neritic calcareous rocks and clastics and flysch in the south, which grades upward into Lower Cretaceous post-flysch. During the Valanginian and the Hauterivian, shoaly limestone and in places also reef and Hauterivian clastics deposited outside the flysch basin. In the Barn.mian, and partly also in the Aptian, reef Urgonian limestone deposited, over which deposited shoaly clastic-calcareous sediments during the Aptian. But on the SW slopes of Suva Planina, the Aptian consists of clastics rich in fauna, whose floor and roof are not known. Albian shale and sandstone with fauna are recognized in a small area. The floor is not visible, and these are unconfolmably overlain by Senonian sediments. The Upper Cretaceous is predominantly developed in the Timok zone, where it consists of sediments and sedimentary-volcanogenic fOlmations of the Maastrichtian. Outside this zone, Senonian transgressive sandstone and conglomerate and Maastrichtian rudist limestone are deposited. The vulcanogenic-sedimentary formations of the Timok zone contain pyroclastics of augite-hornblende and hornblende, andesite and latite, with latite effusions in succession with various sediments. The Palaeogene ("red" and "productive series") iz preserved in the axial part of the Timok zone, where it lies transgressively over Maastrichtian fOlmations. The Koritnik-Babusica bassin also has Upper Oligocene sediments developed. Freshwater Neogene fOlmations are deposited in the basins which are mostly formed under the influence of longitudinal dislocations and show many differences in development. Tertiary volcanic rocks consist of amphibole andesite and its tuff in Miocene formations, dacite agglomerate in Miocene-Pliocene sediments, and alkaline gabbroid rocks which penetrate into pre-Miocene sediments. A smaller part of the sheet Bela Palanka belongs to the Serbian-Maceodnian massif and its greater part to the Carpato-Balkanides. Six structural units are separated (Morava, Luinica, Gornjani-Suva Planina, Kueaj -Svrljig, Timok and Tupiznica-Tepos units) which are separated by markable longitudinal dislocations. Translated by D. Mijovic-Pilic 64
Page 1 and 2:
NARODNA ODBRANA SLUZBENA TAJNA POVE
Page 3 and 4:
REDAKCIONI ODBOR: Milorad Dimitrije
Page 5 and 6:
SADR2AJ J UVOD 5 GEOGRAFSKI PREGLED
Page 7 and 8:
GEOGRAFSKI PREGLED List Bela Palank
Page 9 and 10:
PREGLED RANIJIH ISTRAtlVANJA Podaci
Page 11 and 12:
OP~TI PRIKAZ GEOLO~KE GRADE Terenu
Page 13 and 14: slozenom tektonskom gradom. Izdvoje
Page 15 and 16: - U okviru mezozojskih tvorevina po
Page 17 and 18: pre1aznih predstavnika ka srednjete
Page 19 and 20: epidot-hloritskim skriljcima. Medu
Page 21 and 22: U mineralni sastav plagiogranita ul
Page 23 and 24: eara, dok su u gornjem delu alevrol
Page 25 and 26: Dijabazi su zahvaceni istim automor
Page 27 and 28: su zajednicki odvojeni oksfordski i
Page 29 and 30: mikritskim i oosparitskim kreenjaci
Page 31 and 32: DONjA KREDA Sedimenti donje krede z
Page 33 and 34: obodu Koritnieko-babusniekog basena
Page 35 and 36: U blizini Krcimira u klasticnim tvo
Page 37 and 38: Ove stene cesce se pojavljuju sever
Page 39 and 40: .. L£SKOVACKI BASEN BAR8ESKI BAS£
Page 41 and 42: Hornblenda-biotitski daciti ( IXq)
Page 43 and 44: CIPW-Laeroix stena je bliska prelaz
Page 45 and 46: Heine valutaka. Pored njih ima i za
Page 47 and 48: citavim sklopom longitudinalnih raz
Page 49 and 50: U gradi ove zone ucestvuju tvorevin
Page 51 and 52: Koritnicko-lmnicka dislokacija je s
Page 53 and 54: MINERALNE SIROVINE Na terenu lista
Page 55 and 56: krecnjaci i brece, kao i miocenski
Page 57 and 58: ISTORIJA STVARANJA TERENA Najstarij
Page 59 and 60: Sedimentacija neogenih sedimenata j
Page 61 and 62: Dordevic 2. (1969): 0 BROJU I STRAT
Page 63: Petkovic K. (1938a): IZMENE I DOPUN
Page 67 and 68: LEGEND OF STANDARD MAP DENOTATIONS
Page 69 and 70: OTJlOmeIilUl BepJalerO oJllrrollell
show all

BELA PALAIKA

Create successful ePaper yourself

Delete template?

Save as template?