DOCSLIB.ORG

Full Page Photo

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Full Page Photo GEOLOGICA BALCANICA. 26. 2, Sofia, Jun. 1996, p. 63-80 Tectonic Sites of Special Scientific Importance (TSSSI) in tbe Mid -Cretaceous Strouma Superunit, Southwest Bulgaria Jl·an S. Zagorchev Geologica/Institute, Bulgarian Academy of Sciences, Acad G.Bonche~ St. build. 24. 11/3 Sofw. Bulgaria Ja~op'U!e- Te~emOHU'4eCICUe o6&eiC111bl cne&~UaAbHO ­ Abstract. The Mid-Cretaceous tectonic structure of ~ IUJY~Utozo 3Ha'4eHwr e cpedHeMeAoeou CmpyMciCou Southwest Bulgaria consists of the parautochthonous ~.JOzo-JanadHa.Ji E011zapwr. Cpe.llHeMenoaoe Te&­ Strouma Superunit and the allochthonous Morava ecaoe CTJ)OCHHe 10r0-3808,1lHOI Jio.nrapHH COCTO­ Superunit. Five sections represent excellent exposures of :U 10 napaaTOXTOHHol Crp)'Mcaoll e.llBRHilW H aJIJIOX- unique tectonic features. They should be protected by the A Mopaacaol e.llHHHUbl. IbTb p83peJoB BbiJIBnll- State, and conserved in a manner suitable for preservation 11:7 )'Blll:&nbHble TeKTORH'IeCa:He OC06tHHOCTH. 0HH as well as for educational and scientific purposes . .JOID"Hbl 6b1Tb DOCT&BneHbl DO.ll JllU.lHTOA rocy.llapcna, • cepsHpOBaHiol Taa:HM cnoco6oM 'ITOObl o6ecne'tHTb toXpaHeHlle .11M H8}"1HWX Hccne,nOBaHHA H ,lleMOHCT­ C yqe6Hol uenbiO. b:gorchev, I. - Tectonic Sites of Special Scientific Importance (TSSSI) in the Mid-Cretaceous uma Superunit, Southwest Bulgaria. - Geologica Bale., 26, 2; 63-80. ~· words: geological heritage; Southwest Bulgaria; tectonic sites Introduction Geological setting present paper aims to draw the attention Strouma Superunit ds five geological sites that should be "dered as Sites of Special Scientific The Strouma Superunit (Strumicum; Trun­ portance (SSSI) and placed under the VIahina structural zone - Zagorchev, 1984, ection of the State. They have a complex 1990) is a parautochthonous element (Fig. I) of mostly tectonic character, and exhibit the Mid-Cretaceous ("Austrian") structure of rtant relations between different geological Bulgaria that has been included in the Late ·es being also (in some cases) stratotypes of Cretaceous Morava-Rhodope structural zone al lithostratigraphic units. These sites are (Boyanov et al., 1989). After the main Mid­ tg. 1): I. Road cut south of the village of Cretaceous folding, the formations of the .urvodol; 2. Road cut near the village of Superunit have been covered in Mid-Cretaceous Gurbino; 3. Road cut west of the village of time by the thrust sheets of the Morava yantsi; 4. Ravine near the village ofPoletintsi, Superunit, and furthermore, folded together in confluent of the river Poletinski-dol; 5. Road Late Cretaceous time, and covered (sealed) by near the village of Tsurvishte. Paleogene sedimentary and volcano-sedimen­ These sites should certainly be included in tary formations. · e Bulgarian Geological Heritage List (Bulg The pre-Permian basement of the Strouma (jlfl.) and the Balkan GHL. Some of them may Superunit is of Vlahina type. It is built up of considered as candidates for the European biotite and two-mica gneisses and migmatites GHL, and even for the World GHL. interlayered by amphibolites and quartzo- 63 i~- · ~- .1,. ..... -., j _l ,. ....- · Fig. 1. Sketch map for the position of the tectonic SSSI in the Strouma Superunit. 1 -Alpine plutons; 2- Hercynian granitoid plutons; 3- 5 - southern part of the Srednogorie Superunit: 3 - Melovete (MU) and Radomir (RU) units, 4 - Lyubash and Golo-Burdo units, 5 - Viskyar-Vitosha part; 6 - Louzhnitsa-Trun Unit of the Strouma Superunit; 7 - Osogovo-Vlahina Unit of the Strouma Superunit; 8 - diabase-phyllitoid complexes (mainly Frolosb Formation) of the pre-Alpine basement; 9- Rhodopian Supergroup from the Pirin Unit; 10 - Rhodopian Supergroup of the West-Rita Unit; 11- Ograzhdenian Supergroup from the ~, Kapatnik Unit; 12- Osogovo Formation of the Osogovo l£:3z Subunit, Osogovo-Vlahina Unit; 13 - 14 - Morava Superunit: 13-external thrust units with Paleozoic section ~3 [q:@~f), ~II of Kouchay type (SK- Strumolska klippe, VK- Vlashki­ ~' ~. ~12 ,,.:-, 15 kamak klippe, RN - Rizovtsi thrust sheet), 14- internal thrust units with high-grade metamorphic formations; 15 ~s !lmmg§3r3~r5 - Poletintsi-Skrino fold-thrust zone; 16 -thrusts (a) and ~6 ~.,E:J" ,TS 11 faults (b); 17- tectonic SSSI: SR- section Rayantsi, GT 0 5 1P 15 20km - Gurbino thrust, SP - Section Poletinski-dol, MA­ Murvodol anticlinaloid, TS - Tsurvishte thrust feldspathic gneisses. They are referred to the of the Petrohan Terrigenous Group. The next Precambrian Ograzhdenian Supergroup. This lskur Carbonate Group (Tronkov, 1983) covers amphibolite-facies basement is covered with a the interval from the Spathian (uppermost Lower primary depositional contact (primary uncon­ Triassic) to the Norian, and consists mainly of formity later reworked both tectonically and limestones and dolomites with local marly and metamorphically) by the so-called diabase­ shaly interbeds. The Moesian Group (Norian) phyllitoid complex (Frolosh Formation) built up is represented by marine red beds : shales with of metadiabases, green rocks, actinolite and infrequent limestone interbeds (with Norian chlorite schists, metakeratophyres, etc. that foraminifers) and irregular bodies of underwent a greenschist-facies metamorphism. conglomerates built up predominantly by The rocks of the Frolosh Formation are intruded pebbles of Triassic limestones and dolomites. by the rocks of the Strouma diorite formation, Jurassic formations occur only in the northern with a probable early Paleozoic age. parts (Louzhnitsa- Trun Unit) of the Strouma Permian red beds of the Skrino and Eroul Superunit, to the North of the Poletintsi - Formations (Zagorchev, 1980, 1995) cover with Skrino fold-thrust zone. The usual development unconformable depositional contact all pre­ (Sapunov et al., 1983, 1985; Dodekova et al., Permian rocks and formations listed. The basal 1984) consists of a continental Zhablyano conglomerates contain pebbles of the pre­ Formation (shales, oligomictic quartz sand­ Permian rocks. The thickness is irregular. In stones, conglomerates, with interbeds of black some parts of the superunit, the Permian coal) of Lower Pliensbachian age, followed by deposits are lacking most probably due to the marine Ozirovo Formation (sandy biodetrital primary causes (non-deposition), and the pre­ limestones and calcareous sandstones; Permian basement is covered directly by the Pliensbachian - Lower Toarcian), Gradets basal conglomerates of the Lower Triassic. The Formation (oligomictic quartz sandstones; Lower Triassic is represented mostly by red beds Upper Toarcian -Bajocian), Polaten Formation 64 (biodetrital and oolithic limestones; Aalenian - greenschtst-facies metamorphism; intruding pre­ Lower Bathonian), Yavorets Formation (micritic Permian basic and granitoid rocks; ii) Vlasina and biodetrital limestones with flint nodules; type: amphibolite-facies metamorphic rocks of Middle Callovian - Oxfordian), Gintsi the Dragoychintsi Formation covered by Formation (nodular limestones, often of the metapsammites, metapelites, marbles and "ammonitico rosso" type; Lower Oxfordian - metaphosphorites (Cheshlyantsi Formation) of Lower Kimmeridgian), Neshkovtsi Formation Ordovician age; and iii) Eleshnitsa type: (calcareous shales and marls with some Precambrian? amphibolite-facies metamorphic limestones and sandstones) and Kostel For­ rocks covered by metadiabases, metatuffs and mation (coarse flysch in transition to sandy metaterrigeneous rocks (Zhdrapanitsa Forma­ flysch). The section is ending with a calcareous tion) of Vendian - Early Paleozoic age, and post-flysch with Lower to Middle Berriasian age. graphite-bearing micaschists, quartzous schists, A specific development in a part of the superunit quartzites and limestones (Ruzhcha Formation) is represented by limestone breccia and with recently proven Silurian to Early Devonian conglomerate and micritic limestone (Lobosh age. Formation) in lateral interfingering with the The rocks of the Morava Superunit repre­ limestones of the Y avorets and Gintsi sented the basement of an Early Alpine (Triassic Formations. -Jurassic to Early Cretaceous?) sedimentation Another and very specific Jurassic section zone that possibly was a part of the continental (Treklyano Group) crops out only in the slope towards the Vardar ocean or a very deep westernmost parts of the Louzhnitsa-Trun Unit, gulf of that ocean (Zagorchev, 1986). It has been beneath the thrust sheets (Penkyovtsi and folded and thrusted to the north-east over the Poletintsi thrusts) of the Morava Superunit. The folded Strouma Superunit in Mid-Cretaceous Treklyano Group consists of polymictic time. conglomerates, olistostromes and sandstones (at the base) and interbedding of slates and Murvodol anticlinaloid (MA) radiolarites. Laterally they pass into a shaly formation with sandstone and limestone The Murvodol anticlinaloid (Figs. 2 - 7) is a interbeds. The beds of the Treklyano Group striking example of antiformal syncline cover with depositional contact and (anticlinaloid). It is situated South of the village unconformity the Norian red beds (Komshtitsa of Murvodol, the core cropping out in the stream Formation), and are covered by the flysch of and its eastern bank. The southern limb of the the Kostel Formation. structure is well exposed along the country-road The whole Mesozoic section of the Strouma towards the hamlet Vodenicharska-mahala of Superunit has been folded in Mid -Cretaceous the village of Pastouh, and is covered near that time, and different levels of the eroded section hamlet by the thrust sheet of the Skrino thrust built
Load more

Recommended publications
  • Annex REPORT for 2019 UNDER the “HEALTH CARE” PRIORITY of the NATIONAL ROMA INTEGRATION STRATEGY of the REPUBLIC of BULGAR
    Annex REPORT FOR 2019 UNDER THE “HEALTH CARE” PRIORITY of the NATIONAL ROMA INTEGRATION STRATEGY OF THE REPUBLIC OF BULGARIA 2012 - 2020 Operational objective: A national monitoring progress report has been prepared for implementation of Measure 1.1.2. “Performing obstetric and gynaecological examinations with mobile offices in settlements with compact Roma population”. During the period 01.07—20.11.2019, a total of 2,261 prophylactic medical examinations were carried out with the four mobile gynaecological offices to uninsured persons of Roma origin and to persons with difficult access to medical facilities, as 951 women were diagnosed with diseases. The implementation of the activity for each Regional Health Inspectorate is in accordance with an order of the Minister of Health to carry out not less than 500 examinations with each mobile gynaecological office. Financial resources of BGN 12,500 were allocated for each mobile unit, totalling BGN 50,000 for the four units. During the reporting period, the mobile gynecological offices were divided into four areas: Varna (the city of Varna, the village of Kamenar, the town of Ignatievo, the village of Staro Oryahovo, the village of Sindel, the village of Dubravino, the town of Provadia, the town of Devnya, the town of Suvorovo, the village of Chernevo, the town of Valchi Dol); Silistra (Tutrakan Municipality– the town of Tutrakan, the village of Tsar Samuel, the village of Nova Cherna, the village of Staro Selo, the village of Belitsa, the village of Preslavtsi, the village of Tarnovtsi,
    [Show full text]
  • 1 I. ANNEXES 1 Annex 6. Map and List of Rural Municipalities in Bulgaria
    I. ANNEXES 1 Annex 6. Map and list of rural municipalities in Bulgaria (according to statistical definition). 1 List of rural municipalities in Bulgaria District District District District District District /Municipality /Municipality /Municipality /Municipality /Municipality /Municipality Blagoevgrad Vidin Lovech Plovdiv Smolyan Targovishte Bansko Belogradchik Apriltsi Brezovo Banite Antonovo Belitsa Boynitsa Letnitsa Kaloyanovo Borino Omurtag Gotse Delchev Bregovo Lukovit Karlovo Devin Opaka Garmen Gramada Teteven Krichim Dospat Popovo Kresna Dimovo Troyan Kuklen Zlatograd Haskovo Petrich Kula Ugarchin Laki Madan Ivaylovgrad Razlog Makresh Yablanitsa Maritsa Nedelino Lyubimets Sandanski Novo Selo Montana Perushtitsa Rudozem Madzharovo Satovcha Ruzhintsi Berkovitsa Parvomay Chepelare Mineralni bani Simitli Chuprene Boychinovtsi Rakovski Sofia - district Svilengrad Strumyani Vratsa Brusartsi Rodopi Anton Simeonovgrad Hadzhidimovo Borovan Varshets Sadovo Bozhurishte Stambolovo Yakoruda Byala Slatina Valchedram Sopot Botevgrad Topolovgrad Burgas Knezha Georgi Damyanovo Stamboliyski Godech Harmanli Aitos Kozloduy Lom Saedinenie Gorna Malina Shumen Kameno Krivodol Medkovets Hisarya Dolna banya Veliki Preslav Karnobat Mezdra Chiprovtsi Razgrad Dragoman Venets Malko Tarnovo Mizia Yakimovo Zavet Elin Pelin Varbitsa Nesebar Oryahovo Pazardzhik Isperih Etropole Kaolinovo Pomorie Roman Batak Kubrat Zlatitsa Kaspichan Primorsko Hayredin Belovo Loznitsa Ihtiman Nikola Kozlevo Ruen Gabrovo Bratsigovo Samuil Koprivshtitsa Novi Pazar Sozopol Dryanovo
    [Show full text]
  • Priority Public Investments for Wastewater Treatment and Landfill of Waste
    Environmentally and Socially Sustainable Develonment Europe and Central Asia Region 32051 BULGARIA Public Disclosure Authorized ENVIRONMENTAL SEQUENCING STRATEGIES FOR EU ACCESSION PriorityPublic Investments for Wastewater Treatment and Landfill of Waste *t~~~~~~~~~~~~~~~~~~~~~~~ Public Disclosure Authorized IC- - ; s - o Fk - L - -. Public Disclosure Authorized The World Bank Public Disclosure Authorized May 2004 - "Wo BULGARIA ENVIRONMENTAL SEQUENCING STRATEGIES FOR EU ACCESSION Priority Public Investments for Wastewater Treatment and Landfill of Waste May 2004 Environmentally and Socially Sustainable Development Europe and Central Asia Region Report No. 27770 - BUL Thefindings, interpretationsand conclusions expressed here are those of the author(s) and do not necessarily reflect the views of the Board of Executive Directors of the World Bank or the governments they represent. Coverphoto is kindly provided by the external communication office of the World Bank County Office in Bulgaria. The report is printed on 30% post consumer recycledpaper. TABLE OF CONTENTS Acknowledgements ..................................................................... i Abbreviations and Acronyms ..................................................................... ii Summary ..................................................................... iiM Introduction.iii Wastewater.iv InstitutionalIssues .xvi Recommendations........... xvii Introduction ...................................................................... 1 Part I: The Strategic Settings for
    [Show full text]
  • In Bulgaria – Plovdiv
    ECOLOGIA BALKANICA International Scientific Research Journal of Ecology Special Edition 2 2019 Eight International Conference of FMNS (FMNS-2019) Modern Trends in Sciences South-West University “Neofit Rilski”, Faculty of Mathematics & Natural Sciences Blagoevgrad, Bulgaria, 26-30 June, 2019 UNION OF SCIENTISTS IN BULGARIA – PLOVDIV UNIVERSITY OF PLOVDIV PUBLISHING HOUSE ii International Standard Serial Number Online ISSN 1313-9940; Print ISSN 1314-0213 (from 2009-2015) Aim & Scope „Ecologia Balkanica” is an international scientific journal, in which original research articles in various fields of Ecology are published, including ecology and conservation of microorganisms, plants, aquatic and terrestrial animals, physiological ecology, behavioural ecology, population ecology, population genetics, community ecology, plant-animal interactions, ecosystem ecology, parasitology, animal evolution, ecological monitoring and bioindication, landscape and urban ecology, conservation ecology, as well as new methodical contributions in ecology. The journal is dedicated to publish studies conducted on the Balkans and Europe. Studies conducted anywhere else in the World may be accepted only as an exception after decision of the Editorial Board and the Editor-In-Chief. Published by the Union of Scientists in Bulgaria – Plovdiv and the University of Plovdiv Publishing house – twice a year. Language: English. Peer review process All articles included in “Ecologia Balkanica” are peer reviewed. Submitted manuscripts are sent to two or three independent peer reviewers, unless they are either out of scope or below threshold for the journal. These manuscripts will generally be reviewed by experts with the aim of reaching a first decision as soon as possible. The journal uses the double anonymity standard for the peer-review process.
    [Show full text]
  • Full Page Photo
    GEOLOGICA BALCANICA, 31. 1-2, Sofia, Jun. 2001, p. 3-52 Introduction to the geology of SW Bulgaria Ivan Zagorchev Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia; E-mail [email protected] H. 3acop'leB - BeeoeHue K ceoAozuu 10zo-3anaoHoii Abstract. The geologic structure of Southwest Bulgaria is EoAzapuu. reonorK'feCKOe CTpOeHKe IOro-3ana.nHOH characterized by a complex Mid-Cretaceous pile of thrust DOJJrapKK COCTOKT KJ CJJO)f(HOrO cpe.nHeMeJJOBOrO Har­ sheets, a complex system of horsts and grabens of Palaeo­ pOMO)f(.neHK~ Ha.nBKfOBbiX nJTaCTKH, KOMnJTeKCROH CHC­ gene age, and a neotectonic (Neogene - Quaternary) pat­ TeMbl na.neoreHOBbiX ropCTOB K rpa6eHOB, H HJ HeOTeK­ tern dominated by the Strouma rift system and the Serbo­ TOHK'feCKOrO (ReoreH - 'feTBepTH'fHblH) pHCYHKa .nOMH­ Macedonian neotectonic swell. HHpyeMOfO CTpYMCKOH pHQlTOBOH cHcTeMoH H Cep6o­ Amphibolite-facies metamorphic rocks belong to the MaKe.noHCKKM neoTeKTOHH'feCKHM aa.noM. Ograzhdenian (Prerhodopian) and Rhodopian Super­ MeTaMopQ>H'feCKHe nopo.nbr aMQ>H6oJTHTOBOH Q>aUHK group and the Osogovo "Formation". The last intensive npuna.nne)f(aT K Orpa)f(.neHCKOH (Tipepo.noncKoii) K Po­ metamorphic event is proven to be of Cadomian age, and .noncKOH cyneprpynnaM H K OcoroBCKOH ,caHTe". Tioc­ later superimposed metamorphic and deformation events ne.nHee HHTeHCHBHOe MeTaMopQ>H'feCKOe C06b!THe - Ka­ have had a local occurrence. The greenschist-facies Frol­ .nOMCKOrO BOJpacTa, a 6onee TIOJ.nHHe, HaJIO)f(eHHble Me­ osh Formation (Vendian - Lower Cambrian) has a dia­ TaMOpQ>K'feCKHe H .neQ>OpMaUHORHble C06b!TH~, 6bJJJH base-phyllitoid composition and is typical for the Strou­ JTOKaJibHOrO JHa'feHK~ K pacnpOCTpaHeHH~ .
    [Show full text]
  • Some Rare and Noteworthy Larger Fungi in Bulgaria
    10 years - ANNIVERSARY EDITION TRAKIA JOURNAL OF SCIENCES Trakia Journal of Sciences, Vol. 10, No 2, pp 1-9, 2012 Copyright © 2012 Trakia University Available online at: http://www.uni-sz.bg ISSN 1313-7050 (print) ISSN 1313-3551 (online) Original Contribution SOME RARE AND NOTEWORTHY LARGER FUNGI IN BULGARIA B. Assyov*, D. Y. Stoykov, M. Gyosheva Department of Plant and Fungal Diversity and Resources, Institute of Biodiversity and Ecosystem Research, Bulgarian Academy of Sciences, Sofia, Bulgaria ABSTRACT The paper reports 23 rare and noteworthy Bulgarian larger fungi including the confirmation of the presence of Paxillus rubicundulus in the country and the second records of Cantharellus pallens, Crinipellis mauretanica, Ditiola peziziformis, Geopora arenicola, Laccaria proxima, Marasmius collinus and Pterula multifida. Brief descriptions are provided for Cantharellus pallens, Ditiola peziziformis, Geopora arenicola, Gymnopus quercophilus, Marasmius collinus, and Paxillus rubicundulus based upon the Bulgarian specimens. Geopora arenicola, Trichoglossum hirsutum var. hirsutum, Cantharellus amethysteus, C. pallens, Laccaria proxima and Paxillus rubicundulus are illustrated. In addition, new collections of some threatened, rare and less known species are also included. Key words: ascomycetes, basidiomycetes, Bulgarian mycota, fungal conservation, larger fungi INTRODUCTION the determination are listed under every Recording of fungi is an important task which particular taxon as ‘Reference literature’. serves different scientific and practical purposes. Some peculiarities of the Bulgarian The microscopic examination of fungi was mycological literature were reviewed by conducted in water and 5% KOH. The Denchev & Bakalova (1), who found a pattern amyloidity was tested with Melzer’s solution suggesting that possibly many species might be (recipe after 5). under-recorded.
    [Show full text]
  • Republic of Bulgaria Ministry of Finance
    REPUBLIC OF BULGARIA MINISTRY OF FINANCE ORDER № ZMF-70 Sofia, 01.02.2021 Pursuant to Art. 183, para. 1 in connection with para. 5 and Art. 184, item 1 of the Corporate Income Tax Act I ORDER: I determine a list of municipalities with unemployment with or over 25% higher than the national average for 2020. The order to be promulgated in the State gazette and to be published on the website of the Ministry of Finance. I assign the control over the execution of the order to the director of the Tax Policy Directorate. MINISTER: KIRIL ANANIEV LIST OF MUNICIPALITIES WITH AN UNEMPLOYMENT RATE OF 25 PERCENT EQUAL TO OR HIGHER THAN THE NATIONAL AVERAGE FOR 2020 № per line District / Municipality Unemployment rate I. Blagoevgrad District 1. Bansko 12,70 2. Belitsa 38,42 3. Garmen 14,59 4. Kresna 11,27 5. Petrich 10,35 6. Razlog 12,95 7. Satovcha 14,09 8. Simitli 14,42 9. Strumyani 20,65 10. Hadzhidimovo 13,49 11. Yakoruda 30,78 II. Burgas District 1. Ruen 13,75 2. Sredets 16,18 3. Sungurlare 10,90 III. Varna District 1. Avren 13,28 2. Byala 9,98 3. Vetrino 12,24 4. Valchi dol 20,75 5. Dolni Chiflik 14,94 6. Dalgopol 20,80 7. Provadiya 10,42 8. Suvorovo 11,39 IV. Veliko Tarnovo District 1. Elena 11,58 2. Zlataritsa 19,27 3. Polski Trambesh 12,39 4. Strazhitsa 17,09 5. Suhindol 14,52 V. Vidin District 1. Belogradchik 18,55 2. Boynitsa 14,22 3.
    [Show full text]
  • Full Page Photo
    GEOLOGICA BALCANICA, 28. 1-2, Sofia, August. 1998, p. 35-43 ewly recognized Upper Triassic and Jurassic formations in Southwest Bulgaria: palaeogeographic and palaeogeodynamic implications h an Zagorchev, Ekaterina Trifonova, Kiril Budurov, Kristalina Stoykova Geological Institute. Bulgarian Academy ofSciences , 1113 Sofia; ; tf [email protected]; [email protected] iued 03.07.1998: accepted for publication: 03.07. /998) 3acop'4e6. E. Tpu¢oHo6a, K. Eyoypo6, K. CmouKoBa - Abstract. Four formal lithostratigraphic units are introduced for ~HapyxeHHble BepxHempuacOBble u IOpcKue cBumbl 6 the first time in the national stratigraphic nomenclature in Lko-JanaOHou Eolli!apuu: naAeoceozpa¢u'4ecKue u naAeo­ accordance with the National Stratigraphic Code and the Inte­ ~aMu'lecKue 6bl600bl. qeTblpe o<tJKUHIUlbHble JlKTO· rnational Stratigraphic Guide. ~a4JH'feCKHe ellHHHUbl BBOllliTCll BDepsble B HaUHO· The Upper Triassic Kobile Formation is situated at the top of ZLiloB)'10 CTJ'8THrpa4JK'feCK)'IO HOMCHKJiaT:ypy, B COOTBCT· the Triassic section (over the red beds of the Norian Komshtitsa c HauHOHBJibHblM CTJ'BTHrpa<tJH<tCCKHM JCOllCJCCOM H c Formation). It consists of phosphate- and sulphate-bearing l*:&.:t)'llapOllHbiM CTJ)aTHrpa<tJH<tCCJCHM pyJCOBOllCTBOM. yellowish sandstone and siltstone interbedded with grey Bepue-rpHacosall Ko6HJJCKall CBHTa pacnonaraeTCll B ca­ limestone and dolomitic limestone. Occasionally, they contain .:p~ TJ)HaCOBOfO pa3pC3a, Hall HOpCICOH KOMWTHUJ:OK echinids, gastropods, crinoid ossicles, algae and foraminifers . a.TOi. 01:1a COCTOHT HJ 4Joc4JaT· H C)'Jib4JaT-COllCpliCalllHX The Metohiya Formation (basal conglomerate built up of -=.c:t OIIilThlX DCC'iaHHICOB HanespOJIKTOB nepecnaHBaiOlllHXCll quartz and lydite pebbles; quartz sandstone; loose yellowish api10i11 113BeCTHJIJCaMH HllOJIOMHTOBhiMH H3BCCTHJIIC&MH. sandstones and occasional limestone interbeds) covers the Upper li=cTa.wH OHH COllepJKaT 3XHHHllbl, raCTJ)ODOllbl, 'lJICH'fHXH Triassic with unconformable depositional contact.
    [Show full text]
  • Kyustendil District
    Kyustendil District Treklyano > Population (2015) 126,992 > Area (sq. km) 3,051.5 KYUSTENDIL Bobov dol SAPAREVA BANYA > Number of settlements 183 NEVESTINO DUPNITSA > Share of urban population (%) 69.1 BOBOSHEVO RILA KOCHERINOVO Overview lthough living conditions and social inclusion have deteriorate. The educational system has been successful in gradually been improving, salaries in the district have enrolling a great part of those subject to compulsory edu- Astayed low, while a considerable part of total households’ cation, though quality of education has been relatively low. incomes was generated by pensions. In 2015, unemploy- There has been a certain shortage of specialist doctors in ment fell and employment rose for the first time after the the district but the number of hospital beds is sufficient and crisis; both indicators, however, were still below the national the share of health-insured persons is high. Kyustendil has average levels. Kyustendil is among the districts which have received the second lowest rating after Sofia (capital city) for attracted least FDI so far and whose municipalities have uti- security and justice because of high crime rates, slow justice lized the least amount of EU funds. The rate of local taxes administration, and low crime clearance rate. In the “Envi- and fees was among the lowest in the country, yet, the ab- ronment” category, the district is characterized by good sence of transparency of local administrations has made the connectivity to public sewerage systems and wastewater district less attractive in comparison with others. treatment plants on one hand, and, by strongly polluted air, As a result of the unfavorable demographic tendencies, the on the other.
    [Show full text]
  • Annexes to Rural Development Programme
    ANNEXES TO RURAL DEVELOPMENT PROGRAMME (2007-2013) TABLE OF CONTENTS Annex 1 ...........................................................................................................................................4 Information on the Consultation Process ........................................................................................4 Annex 2 .........................................................................................................................................13 Organisations and Institutions Invited to the Monitoring Committee of the Implementation of the Rural Development Programme 2007-2013 .................................................................................13 Annex 3 .........................................................................................................................................16 Baseline, Output, Result and Impact Indicators............................................................................16 Annex 4 .........................................................................................................................................29 Annexes to the Axis 1 Measures...................................................................................................29 Attachment 1 (Measure 121 Modernisation of Agricultural Holding) .........................................30 List of Newly Introduced Community Standards .........................................................................30 Attachment 1.A. (Measure 121 Modernisation of Agricultural Holding
    [Show full text]
  • Agri-Ecological Zoning of Municipalities in the Kyustendil Region
    3rd INTERNATIONAL SYMPOSIUM FOR AGRICULTURE AND FOOD – ISAF 2017 __________________________________________________________________________________ AGRI-ECOLOGICAL ZONING OF MUNICIPALITIES IN THE KYUSTENDIL REGION Martin Banov, Veneta Krasteva, Nevena Miteva, Svetla Marinova Institute of soil Science Agrotechnologies and Plant Protection Nikola Poushkarov, Sofia, Bulgaria Corresponding author: [email protected] Abstract It has been done agroecological zoning of nine municipalities in Kyustendil area - Bobovdol, Boboshevo, Kocherinovo, Kyustendil, Nevestino, Rila, Sapareva bania, Dupnitza and Treklyano. Agro- ecological zoning is done based on certain environmental characteristics, basic of which are: prevailing soil type; an extreme manifestation of certain climatic factors; altitude; relief features and other. In the presented paper were analyzed and described: weather conditions; soil resources; agronomic suitability of land for organic growing of suitable for the region crops. There were considered the potential threats of soil erosion, acidification and compaction. It was prepared land evaluation regarding the potential for growing grape and fruit, vegetable crops, meadows and pastures. It was found that the areas with altitude above 800 m are unsuitable for cultivation with fruit crops, which can be planted in areas with an altitude of 1800 m. Vegetable crops are not suitable to be cultivated in areas with altitude above 800 m are with the exception of late potatoes which may be planted in places with an altitude of 1800 m. It was found that the areas with altitude above 800 m are unsuitable for growing vines. The territories with altitude above 2400m are unusable for grassland. Keywords: weather conditions; soil resources, agronomic suitability, land evaluation. Intrduction Agricultural practices are certainly one of the most important factors in the evolution of mankind.
    [Show full text]
  • BICA's Brochure
    www.bica-bg.org Bulgarian Industrial Capital Association (BICA) is the most representative union of Bulgarian employers. Founded in 1996, today the Association has gained reputation in the field of business, social partnership and public area in general. Currently, there are over 80 branch chambers and organisations that are members of the Association, as well as 10 000 enterprises that employ 500 000 workers. BICA also has a welldeveloped network of regional chambers in 171 municipalities throughout the country. The Bulgarian Industrial Capital Association has affirmed the reputation of a speaker for the real manufacturing sector. It represents the interests of its members before the executive and legislative authorities at national and European level, influences the preparation of the legal framework and policies in the socio - economic sphere, endeavours to improve the competitiveness of Bulgarian enterprises and to create a favourable business environment, as well as to accelerate the development of the Bulgarian economy. Throughout the years, the Association has formulated consistent policies and has implemented them through systematic actions. It has built on the achieved results and has been equally unbiased and independent of all political parties. BICA is the only organisation that incorporates listed companies and providers operating in the field of Services of general interest in the country. The Association is permanently committed to the development of the capital markets, and makes constant efforts toward the positive perception of issuers’ status. The Association works in this direction in close collaboration with the investment community and institutions at national and European level. The Association continues to expand its international presence and positions.
    [Show full text]