Geology Of Bulgaria


The geology of bulgaria consists of two major structural features. The Rhodope Massif in southern Bulgaria is made up of Archean, Proterozoic and Cambrian rocks and is a sub-province of the Thracian-Anatolian polymetallic province. It has dropped down, faulted basins filled with Cenozoic sediments and volcanic rocks. A fourth morphotectonic unit, the Kraishtide zone, trends northwest through western Bulgaria and into adjacent Yugoslavia. This rugged area, 15-60 km wide, is a megashear zone within which both right-lateral strike-slip and vertical movements have been common since the Paleozoic. It parallels the better known Vardar zone of Yugoslavia. The low-relief Moesian platform of northern Bulgaria and southern Romania owes its heritage to Hercynian deformation. It is mantled by flat-lying, shelf-type Mesozoic and Tertiary sedimentary (mostly carbonate) rocks. Along its southern boundary a foredeep developed during Jurassic-Cretaceous time in which thick flysch-like sediments accumulated. Bulgaria is in southeastern Europe between reasonably well-described areas of predominantly Alpine crustal deformation on the north and northwest (Carpathians in Romania, Hungary, and Czechoslovakia; Alps in Austria), on the east (Pontides and Taurides in Turkey), and on the west and south (Dinaric Alps in Yugoslavia; Pindos Mountains in Greece) but has not been well described in easily available.

Geologic evolution of Bulgaria in light of plate tectonics - Bulgaria is a country situated in Southeast Europe that occupies the eastern quarter of the Balkan peninsula, being the largest country within its geographic borders Romania to the north, Serbia and North Macedonia to the west, Greece and Turkey to the south, and the Black Sea to the east. The northern border with Romania follows the river Danube until the city of Silistra. geology of bulgaria: a Review. Published 1 February Geology. Bulgaria is in southeastern Europe between reasonably well-described areas of predominantly Alpine crustal deformation on the north and northwest (Carpathians in Romania, Hungary, and Czechoslovakia; Alps in Austria), on the east (Pontides. Bulgaria is a natural geological museum with wonderful rock outcrops of different ages and compositions, from Archean to Quaternary. The complicated geological structure and contrasting relief favour the formation of extraordinary geological and geomorphological phenomena with aesthetic, scientific and educational value. Bulgarian territory presents an extraordinary diversity of landforms produced by various geomorphic systems, in both horizontal and vertical dimensions (Fig. Landform diversity reflects morphostructure development of Bulgaria's territory in a complicated geological setting on the Balkan peninsula between the Eurasian and African lithospheric plates, the long-term geodynamical evolution. The general outline of Bulgarian geology was established during the 19th century by visiting French (Ami Boué, etc. von Hochstetter, etc. Before World War II, Bulgarian geologists conducted their work mainly at the University of Sofia, directed by Stefan Boncev and to a lesser extent at the Bulgarian. Since the advent of the plate tectonic theory three decades ago, numerous controversial and contradicting tectonic models for the structure and geological evolution of Bulgaria have been proposed (Boyanov et aI. , 1989; Dabovski et aI. , 1989; Антова et aI. , 1996 and many others). They are based on the concept that the. The geologic structure of Southwest Bulgaria is characterized by a complex Mid Cretaceous.

Recent Landform Evolution In Bulgaria

The geologic structure of Southwest Bulgaria is characterized by a complex Mid Cretaceous pile of thrust sheets, a complex system of horsts and grabens of Palaeogene age, and a neotectonic (Neogene - Quaternary) pattern dominated by the Strouma rift system and the Serbo-Macedonian neotectonic swell. Amphibolite-facies metamorphic rocks belong to the Ograzhdenian (Prerhodopian) and Rhodopian. Explore Bulgaria Using Google Earth: Google Earth is a free program from Google that allows you to explore satellite images showing the cities and landscapes of Bulgaria and all of Europe in fantastic detail. It works on your desktop computer, tablet, or mobile phone. The images in many areas are detailed enough that you can see houses. Geology museums in Bulgaria‎ (2 P) M. Mining in Bulgaria‎ (2 C) O. Oil fields of Bulgaria‎ (1 P) P. Paleontology in Bulgaria‎ (1 C, 2 P) Pages in category "geology of bulgaria" The following 6 pages are in this category, out of 6 total. This list may not reflect recent changes. geology of bulgaria: A ReviewVolume 59, Issue 2 of American Association of Petroleum Geologists bulletin. Richard Martin Foose. American Association of Petroleum Geologists, Length. Bulg Ac Sci, Sofia, 273 pp (in Bulgarian, Russian and English summaries) Google Scholar Dachev C (1988) Structure of the Earth's crust in Bulgaria. Technika, Sofia, 334 pp (in Bulgarian, English summary) Google Scholar Foose R, Manheim F (1975) geology of bulgaria: a review. In the period 1959-1966 "Works on the geology of bulgaria" were published in five specialized series. Currently, the journal Geologica Balcanica and the series Geochemistry, Mineralogy and Petrology and Engineering Geology and Hydrogeology are published regularly, and the BGD Journal is published jointly with the Bulgarian Geological Society. This map was digitized on screen in MapInfo from scans of the original map entitled "Geological Map of the People's Republic of Bulgaria, 1:500,000 scale", published by the Committee of Geology-Department of Geophysical Prospecting and Geophysical Mapping, Sofia, 1989. Геология на България [geology of bulgaria] by Златарски, Георги; Zlatarski, Georgi (1854-1909) Publication date 1927 Usage Public Domain Mark 1. 0 Topics Bulgaria, Geology, Georgi N. Zlatarski, Георги Златарски (1854-1909) Collection. CONCLUSION This paper on the geology of bulgaria is developed on the premise that gsynclinal sedimentation and orogenic deformation of the Alpine belt of Europe are related to interactions among Europe, Africa and rotating micro- continents in response to sea-floor spreading of the Atlantic. Bulgaria cannot be separated into two micro. Bulgaria is a natural geological museum with wonderful rock outcrops of different ages and compositions, from Archean to Quaternary.

Българско геологическо дружество

Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria Bibliographia balcanica: Geological map of Vol. 39 (1-2)/September 2010 - pp. The geologic structure of Southwest Bulgaria is characterized by a complex Mid Cretaceous pile of thrust sheets, a complex system of horsts and grabens of Palaeogene age, and a neotectonic (Neogene - Quaternary) pattern dominated by the Strouma rift. Download scientific diagram | Geological map of Bulgaria showing the main types of rocks (after Cheshitev and Kanchev, 1989). Legend: 1 -Quaternary sediments; 2 -Neozoic sedimentary rocks; 3. The Geological Institute of the Bulgarian Academy of Science is starting on 17. 2020 an "Isotope Geology" course with Prof. Irena Peytcheva as lecturer.

Rhodope Mountains - Wikipedia - 70th Anniversary of the Geological Institute Zhivko Ivanov Award. Report Geological effects Related to May 22,2012 Pernik earthquake. F or 70 years, the Strashimir Dimitrov Geological Institute (GI) is a leading unit in the division of Earth Sciences at the Bulgarian Academy of Sciences. It conducts scientific and applied research on all important aspects of geological science in Bulgaria. In recent years, the institute has been regarded as the largest national geological research and scientific-expert organization that. Orlova Chuka Cave is a notable cave located in Bulgaria, known for its unique geological formations and historical significance. Orlova Chuka Cave is situated in the northeastern part of Bulgaria, near the town of Russe. It is part of the limestone plateau of the Rusenski Lom Nature Park, which encompasses a diverse range of natural and cultural attractions. Геология на България [geology of bulgaria] by Златарски, Георги; Zlatarski, Georgi (1854-1909) Publication date 1927 Usage Public Domain Mark 1. 0 Topics Bulgaria, Geology, Georgi N. Zlatarski, Георги Златарски (1854-1909) Collection. The Rhodopes are spread over 14,735 square kilometers (5,689 sq mi), of which 12,233 square kilometers (4,723 sq mi) are on Bulgarian territory. They have the greatest extent of any single mountain range in Bulgaria.

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The geology of bulgarian lands was shaped over a period of 3. The country's lands have undergone several stages of geochronological development, namely Precambrian, Paleozoic (when granite plutons were formed in the Rhodopes), Mesozoic (when during the Alpine-Himalayan crimp the Sredna Gora mountain was formed), Cenozoic (when. The Regional geology of bulgaria and the Balkan Peninsula is the basis for all applied geosciences in this country thus representing the bridge from fundamental to applied research. The Department of Geotectonics and Regional geology at the Geological Institute of the Bulgarian Academy of Sciences is founded in 1962 by Academician Prof. Address: Department of Geotectonics and Regional Geology, Geological Institute, Bulgarian Academy of Sciences, Acad. Bonchev Street, Build. 24, 1113 Sofia, Bulgaria Office Phone: (+359-2)979-2212 ; fax: (+359-2)8724638 ; Degrees: M. (Engineer Geologist) 1960,Geology and Exploration of Mineral Deposits. Department of Geology, Paleontology and Fossil Fuels, Faculty of Geology and Geography, Sofia University "St. Kliment Ohridski", 15 Tsar Osvoboditel Blvd. , 1504 Sofia, Bulgaria Time constraints on the geological evolution of the main sedimentary basins and tectono-magmatic events on Livingston Island, South Shetland Archipelago, Antarctica. The geological maps covering the whole territory of Bulgaria in scale 1:500,000, 1: 100,000 and 1:25,The latest geological map of Bulgaria in scale 1: 100,000 has been prepared by following the Methodological guidelines of the State Committee on Geology and has been printed in the period 1989-The existing geological maps, materials and. Find 163 researchers and browse 12 departments, publications, full-texts, contact details and general information related to University of Mining and Geology | Bulgaria |. The geological formation of the Belogradchik Rocks is a result of millions of years of natural processes and various geological events. The rocks are primarily composed of sedimentary rock layers, which were formed during different geological periods. Around 230 million years ago, during the late Triassic period, the region where the. The Bulgarian Chamber of Mining and Geology supports the UN Global Compact and is an active member of the Bulgarian UN Network. Between 50 and 100% of the companies in Bulgaria with businesses in the respective branches of the industry are members of the Chamber. The Chamber members contribute up to 5% of the country's GDP, provide over. geology of bulgaria: A REVIEW [Foose, Richard M & Manheim, Frank] on . *FREE* shipping on qualifying offers. geology of bulgaria: A REVIEW. The Geological Institute is the only national complex geological organisation that systematically acquires knowledge on the geology of bulgaria, said also Prof. The 85th anniversary of Acad. Ivan Zagorchev was also celebrated. He is a respected scientist with worldwide recognition in the field of Earth sciences. Under the dome of the northern wing of Sofia University is situated a museum that throws light into the darkness of the distant geological ages. The Museum of Paleontology and Historical Geology houses in its collection and exposition more than 200 000 fossil specimens, rock samples, and geological maps of Bulgaria and the neighbouring territories. Sedmochislenitsi is a stratiform-stratabound Zn-Pb-Cu-Ag deposit hosted in Triassic carbonates in the NW of Bulgaria. The deposits have been compared to the Alpine-type Zn-Pb deposits of Raibl. Sofia University "St. Kliment Ohridski" Museum of Paleontology and Historical Geology is located within the 5th floor of the North Wing of the Main Building of the University. 15 Tzar Osvoboditel Blvd. За Геологическия институт.

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Earth science mapping has been published by the former Committee of Geology and Mineral Resources and the Geological Institute 'Strashimir Dimitrov', Bulgarian Academy of Sciences (BAS). Several small-scale geological maps, some of recent origin and in English, are available, and a new 1:100,000 scale geological series in 86 sheets was completed in 1998. The Melnik Earth Pyramids (Bulgarian: Мелнишки пирамиди) are rock formations, known as hoodoos, situated at the foothills of the Pirin mountain range in south-western span an area of 17 km 2 near the town of Melnik, Blagoevgrad Province. Reaching a height of up to 100 m these sandstone pyramids are shaped in forms, resembling giant mushrooms, ancient towers and. Title: geology of bulgaria: a Review. The Lom basin, North Bulgarian swell, and Varna trough are other major structural elements within the platform. The Rhodope massif of southern Bulgaria and northern Greece is a rugged mountainous terrain of Precambrian and early Paleozoic crystalline rocks. It is a fragment of a once much larger crustal. The Balkanide is a mobile belt within a micro-continent, which included both the Moesian Platform and Rhodope Massif. This micro-continent was rotated counter-clockwise during the Jurassic mainly in response to the sea-floor spreading of the Vardar ophiolite trough. The rotation led to the consumption of Triassic Tethys along the Dobrogea. Geological map of Bulgaria at 1:100 in E-NE faults have formed at last. 000 scale, Krumovgrad and Sape map sheets, S.

(PDF) Structure and Alpine evolution of Bulgaria - ResearchGate - Petrographic characteristics, block and me- CONCLUSIONS chanical features of the decorative marbles from "Jelezino" deposit. -Rudodobiv, 11, 1-5, 1983 (in Bulg. The geology of bulgaria consists of two major structural features. The Rhodope Massif in southern Bulgaria is made up of Archean, Proterozoic and Cambrian rocks and is a sub-province of the Thracian-Anatolian polymetallic province. It has dropped down, faulted basins filled with Cenozoic sediments and volcanic rocks. The Review of Bulgarian Geological Society (BGS) is a scientific periodical which publishing starts in Its main purpose is to popularize the scientific achievements of Bulgarian and foreign geologists. The publishing is financed by the Bulgarian Geological Society by means of membership dues, sponsorship from BAS and other organizations and companies. The total volume of vitrified high-level waste (HLW) and of intermediate-level wastes containing significant amounts of long-lived alpha emitters, generated over the lifetime of Kozloduy Nuclear Power Plant (NPP), is estimated to be about 2,100 m Selection of a suitable formation to host a deep HLW repository in Bulgaria presents. The Proceedings in the Humanities and Social Sciences of the University of Mining and Geology "St. Ivan Rilski" is a scientific publication of the University of Mining and Geology "St. Ivan Rilski", with an editorial board, included in the National Reference List (NRL) of Contemporary Bulgarian Scientific Publications with Scientific Review maintained by the Minister of Education and. Geologically, Northern Bulgaria is within the ex panse of a platform structure, known as the Moe sian Plate (Atanasov, Bokov, 1983; Dabovski et al. , 2002; Zagorchev, 2009). University of Mining and Geology. University of Mining and Geology (MGU) is located in Sofia, Sofija grad, Bulgaria. It is locally known as Минно-геоложки университет. The university was established in It is accredited by National Evaluation and Accreditation Agency, Bulgaria. Geological map of Bulgaria Map data Scale 1:100,Note Some sheets have col.

3: Geochronology And Geodynamics Of Late Cretaceous

Geologically, Northern Bulgaria is within the ex panse of a platform structure, known as the Moe sian Plate (Atanasov, Bokov, 1983; Dabovski et al. , 2002; Zagorchev, 2009). University of Mining and Geology. University of Mining and Geology (MGU) is located in Sofia, Sofija grad, Bulgaria. It is locally known as Минно-геоложки университет. The university was established in It is accredited by National Evaluation and Accreditation Agency, Bulgaria. Geological map of Bulgaria Map data Scale 1:100,Note Some sheets have col. cross sections, stratigraphic columns, ancillary maps, and location map. Description based on Kârdžali sheet. Browse related items. Start at call number: G6891 . Librarian view | Catkey: 5183739. The Pirin Mountains (Bulgarian: Пирин) are a mountain range in southwestern Bulgaria, with the highest peak, Vihren, at an altitude of 2,914 m (9,560 ft) The range extends about 80 km (50 mi) from the north-west to the south-east and is about 40 km (25 mi) wide, spanning a territory of 2,585 km 2 (998 sq mi). To the north, Pirin is separated from Bulgaria's highest mountain range, the. Bulgaria is located in Europe (Eastern Europe) continent. Exact geographical coordinates, latitude and longitude 43. Mapped location of Bulgaria (N 43° 0' 0", E 25° 0' 0"). Bulgaria is located in the time zone GMTEET. If you want to link to this Bulgaria latitude longitude page, please use the codes provided below!. GEOLOGICA BALCANICA, 1-2, Sofia, Jun. 3-52 Introduction to the geology of SW Bulgaria Ivan Zagorchev Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia; E-mail И. Загорчев - Введение к геологии Юго-Западной Болгарии. Геологическое. Reviews of the Bulgarian Geological Society, 32, 85-Bogdanov B (1960) Geologie und Geduge des .

Geochemistry, Mineralogy and Petrology - Bulgarian Academy of Sciences - Erzgebietes von Madan. Annual of the Higher . Institute of Mining and Geology, 6, 1-2, 3-43. In the period 1959-1966 "Works on the geology of bulgaria" were published in five specialized series. Currently, the journal Geologica Balcanica and the series Geochemistry, Mineralogy and Petrology and Engineering Geology and Hydrogeology are published regularly, and the BGD Journal is published jointly with the Bulgarian Geological Society. The ABTS belt (Popov and Popov, 2000, Popov et al. , 2002) is an L-shaped structure of Late Cretaceous, broadly calc-alkaline, magmatic activity within the Alpine-Carpathian-Balkan orogen of eastern Central can be traced from the North Apuseni Mountains and the Banat region in Romania and Serbia through the Serbian Timok and Ridanj-Krepoljin area to the Srednogorie zone in. The geology of bulgaria consists of two major structural features. The Rhodope Massif in southern Bulgaria is made up of Archean, Proterozoic and Cambrian rocks and is a sub-province of the Thracian-Anatolian polymetallic province. It has dropped down, faulted basins filled with Cenozoic sediments and volcanic rocks.

(PDF) Lower Cretaceous Geology Of Bulgaria

The geology of bulgaria primarily consists of several main morphotectonic forms, three of which span the country from east to west: the Moesian platform, the Balkan mountains, and the Rhodope massif. The other main form is the Kraishtide zone, which leads northwest out of Bulgaria. Lake Bliznaka in the Rila mountains, Bulgaria Moesian. Geologic sketch map of the eastern Rhodope-Thrace region in Bulgaria-Greece (modified from Bonev and Stampfli, 2008). Tectono-stratigraphic columns for the units or areas of the eastern CRB. Geological Institute, Bulgarian Academy of Sciences Acad. Georgi Bonchev Str, bl. 24 1113 Sofia Tel: (+359 2) 979 22 73 E-mail: Treasurer: Radostina Atanassova Geological Institute, Bulgarian Academy of Sciences Acad. Georgi Bonchev Str, bl.

24 Best Geology universities in Bulgaria [2024 Rankings] - - 24 1113 Sofia Tel: (+359 2) 979 22 07 E-mail: . Paleozoic (Silurian and Devonian) cherts from Western Bulgaria occur in three tectonic units: Svoge, Lyubash-Golo Bardo and Morava. The SiO2 content in these rocks varies from 76. Methodius University of Veliko Tarnovo. National Military University "Vasil Levski". Varna Free University "Chernorizets Hrabar". The best cities to study Geology in Bulgaria based on the number of universities and their ranks are Sofia, Plovdiv, Stara Zagora, and Varna. Bulgaria has 5 universities in the overall Times Higher Education World University Rankings. The highest-ranking university in Bulgaria is Medical University of Sofia, which is ranked at number 1201-Choosing where to study for a degree in Bulgaria is one of the biggest decisions you will ever make. THE 's student resources are here to. Home / The University / Faculties / Faculty of Geology and Geography . 1504 Sofia, 15 Tsar Osvoboditel Blvd. Phone: (+359) 2 9308 385 Fax: (+359) 2 9446 487 E-mail: Published: 09/27/2007 12:36 pm Last modified: 03/22/2024 04:41 pm .

Printer-friendly version. Faculty of Geology and Geography. PDF | On Jan 1, 2009, T. Nikolov and others published Lower cretaceous geology of bulgaria | Find, read and cite all the research you need on ResearchGate. In North East Bulgaria the Moesian platform, according Jurassic-Lower Cretaceous sediments, is divided into three major parts. The eastern part is known as the Eastern slope of North Bulgarian arch (Fig. Tjulenovo field is located in the Shabla-Bulgarevo graben area of the Eastern slope of North Bulgarian arch (Fig. The University of Mining and Geology "St. Ivan Rilski" has been an independent educational institution since It has established itself as an academic and research center that provides training in geology, mining, and electrical and mechanical engineering in sixty years of existence. BULGARIAN GEOLOGICAL SOCIETY. ESTABLISHED IN Address: BGS, 1113 Sofia, Geological Institute, Bulgarian Academy of Sciences, Acad. On all geological maps they were assumed as part of the SMM, Ograzden Unit (Zagorchev, 1995) or Ograzhdenian supercomplex (Zagorchev et al. The metamorphic rocks from the Vlahina Mt. The regional geology of Serbia describes the geologic structure and history inside the borders of Serbia.

Category:Geological Maps Of Bulgaria

Committee of Geology and Mineral Resources (1989-1992) Geological Map of Bulgaria on the scale 1:100,000, Sheets Sofia, Pernik, Botevgrad, Ihtiman. Kamenov B (1966) Sofia Coal basin. Vaglishta, 3:3-7 (in Bulgarian) Kamenov B, Kojumdgieva E (1983) Stratigraphy of the Neogene in Sofia basin. Palaeontology, Stratigraphy and Lithology. The University of Mining and Geology St. Ivan Rilski was founded in It is the only university in Bulgaria that offers study programs in this field - some of them are Hydrogeology and Engineering Geology, Applied Geophysics, Geology and Study of Mineral and Energy Resources. More than 30 000 students from Bulgaria and countries around. University of Mining and Geology "St. 1700 Sofia, Bulgaria. Studentski grad, Prof. Secretary of the 65th International Scientific Conference 2022: Eng. Kostadinka Konakchiyska. Phone: (++ 3592) 80 60 209; (+ 359879) 80 79 13 E-mail: . The Moesian Plate, also known as the Moesian Platform, is a microcontinent and crustal block in the southwestern part of the East European Craton. It extends 600 kilometers east to west and up to 300 kilometers north to south and lies beneath Romania and Bulgaria . BULGARIAN GEOLOGICAL SOCIETY. ESTABLISHED IN Address: BGS, 1113 Sofia, Geological Institute, Bulgarian Academy of Sciences, Acad. The Sofia University of Mining and Geology (Bulgarian: Минно-геоложки университет "Свети Йоан Рилски") is a state university in Sofia, Bulgaria, founded in History. The university were established in 1953 as High Mining and Geological Institute - (HMGI) with two faculties - Mining and Metallurgy and. Ohridsk," 15 Tsar Osvoboditel Bd. , BG-1504 Sofia, Bulgaria 4 Research Institute "Geology and Geophysics Geophysics," 23 Sitnyakovo Blvd. , 1505 Sofia, Bulgaria 5 Geological Institute, Bulgarian Academy of Science Sofia, Bulgaria Abstract The late Alpine evolution of the Rhodope Massif in southern Bulgaria and northern. Media in category "Geological maps of Bulgaria" The following 6 files are in this category, out of 6 total. A geological map of Bulgaria of 1964 - 4,160 × 3,005; 2. A geological map of the Principality of Bulgaria and of Eastern Roumelia published by Franz Toula in 4,160 × 3,120; 4. May 25, LAST POST AND FINAL HAZARDS REPORT Hi guys and welcome to my last hazard report and just an overview of Bulgaria's main hazards. This post will combine everything together and just discuss better safety precocious and a better way of handling dangerous weather and geological situations overall. Geological map of Bulgaria 1:100 000; about 90 sheets (cf Fig. 1) in Bulgarian and English version; explicatil•e notes (in Bulgarian, with brief explanation of the general geological features in English) The first 30 sheets of the Geological map of Bulgaria on the scale 1:100 000 already appeared.

Structural Evolution Of The Eastern Balkans (Bulgaria)

Impact of the geological and hydrogeological settings on the radon potential in Bulgaria D. Antonov Aglaida Toteva +5 authors Simeon Valchev Geology, Environmental Science. Explanatory note to the Geological map of the Republic of Bulgaria. Scale 1:50 000, Map sheet Etropole. SRI "Geology and geophysics" JSC, Univ. "Ivan Rilski", 83 p (in Bulgarian. Teconski stroegh ha Bulgaria (East Balkan tectonic zone). In: Tectonic Structure of Bulgaria, Sofia, Technica, 537-543 250 Marine and Petroleum Geology 1996 Volume 13 Number 2 Structural evolution of the eastern Balkans: C. (1977) The Emine Flysch and the olistostromes in the Sliven Balkan PaleontoL Stratigr. CONCLUSION This paper on the geology of bulgaria is developed on the premise that gsynclinal sedimentation and orogenic deformation of the Alpine belt of Europe are related to interactions among Europe, Africa and rotating micro- continents in response to sea-floor spreading of the Atlantic. Bulgaria cannot be separated into two micro. Bulgaria is a natural geological museum with wonderful rock outcrops of different ages and compositions, from Archean to Quaternary. The complicated geological structure and contrasting relief favour the formation of extraordinary geological and geomorphological phenomena with aesthetic, scientific and educational value. Media in category "geology of bulgaria". The following 4 files are in this category, out of 4 total. Belemniti 800 × 600; 197 KB. Boudin in Südbulgarien (Rhodopen). png 537 × 241; 128 KB. Sandstone erosion - Melnik, Pirin, 921 × 600; 191 KB. Download scientific diagram | Geological map of Bulgaria from publication: Geothermal Update for Bulgaria (2000-2005) | Geothermal development in Bulgaria has not marked a significant progress in. The Belogradchik Rocks (Bulgarian: Белоградчишки скали, Belogradchishki skali) are a group of strangely shaped sandstone and conglomerate rock formations located on the western slopes of the Balkan Mountains (Stara Planina) near the town of Belogradchik in northwest rocks vary in color from primarily red to yellow; some of the rocks reach up to 200 m in height. The Balkan fold-thrust belt, exposed in Bulgaria and north-east Serbia, is part of the north-east vergent segment of the bi-vergent Eastern Mediterranean Alpine orogen. It was formed during two … Expand. Bulgarian territory presents an extraordinary diversity of landforms produced by various geomorphic systems, in both horizontal and vertical dimensions (Fig. Landform diversity reflects morphostructure development of Bulgaria's territory in a complicated geological setting on the Balkan peninsula between the Eurasian and African lithospheric plates, the long-term geodynamical evolution. Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria Bibliographia balcanica: Geological map of Vol. 39 (1-2)/September 2010 - pp. The geologic structure of Southwest Bulgaria is characterized by a complex Mid Cretaceous pile of thrust sheets, a complex system of horsts and grabens of Palaeogene age, and a neotectonic (Neogene - Quaternary) pattern dominated by the Strouma rift. Download scientific diagram | Geological map of Bulgaria showing the main types of rocks (after Cheshitev and Kanchev, 1989). Legend: 1 -Quaternary sediments; 2 -Neozoic sedimentary rocks; 3. The Geological Institute of the Bulgarian Academy of Science is starting on 17.

(PDF) Geomorphological Zonation Of Bulgaria. Principles And State Of

Orlova Chuka Cave is a notable cave located in Bulgaria, known for its unique geological formations and historical significance. Orlova Chuka Cave is situated in the northeastern part of Bulgaria, near the town of Russe. It is part of the limestone plateau of the Rusenski Lom Nature Park, which encompasses a diverse range of natural and cultural attractions. Геология на България [geology of bulgaria] by Златарски, Георги; Zlatarski, Georgi (1854-1909) Publication date 1927 Usage Public Domain Mark 1. 0 Topics Bulgaria, Geology, Georgi N. Zlatarski, Георги Златарски (1854-1909) Collection. Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria Bibliographia balcanica: Geological map of Vol. 39 (1-2)/September 2010 - pp. The Rhodopes are spread over 14,735 square kilometers (5,689 sq mi), of which 12,233 square kilometers (4,723 sq mi) are on Bulgarian territory.

Ivan Zagorchev Home Page - Bulgarian Academy of Sciences - They have the greatest extent of any single mountain range in Bulgaria. The mountains are about 240 kilometers (149 mi) long and about 100 to 120 kilometres (62 to 75 mi) wide, with an average altitude. Official Site of the Bulgarian Geological Society (BGS) and Review of the Bulgarian Geological Society. The Srednogorie metallogenic zone in Bulgaria (Fig. 1) is part of the global Tethyan- Eurasian copper Panagyuirishte ore region, the most important element of the Srednogorie metallogenic zone, contains characteristic calc-alkaline magmatism that hosts the Bulgaria's most important economic porphyry and epithermal ore deposits. Geological map of Bulgaria showing the main types of rocks (after Cheshitev and Kanchev, 1989). Legend: 1 - Quaternary . sediments; 2 - Neozoic sedimentary rocks; 3 - Neozoic intrusive rocks. Publication of the monograph „Geography of Bulgaria" in 1997 was followed 5 years later by the new edition of the monograph „Geography of Bulgaria" . Also „Atlas of Eastern and South-eastern Europe" (2004) and „Bulgaria. Current Development and Problems" (Ermann and Ilieva 2006) were published. Bulgaria is rich in sources of mineral water of temperatures in the range of 25 °C-100 °C and various chemical compositions due to diverse geological and hydrogeological conditions. The Chelopech copper-gold mine is located in west-central Bulgaria, 80 km east of Sofia, on the southern flank of the Balkan Range (Fig. 1), adjacent to the towns of Zlatitsa and mineral potential of the Chelopech area was first recognised at the end of 19 th century, and the outcrop area was worked before World War II The Chelopech deposit was re-discovered in 1953, following. The geology of bulgarian lands was shaped over a period of 3. The country's lands have undergone several stages of geochronological development, namely Precambrian, Paleozoic (when granite plutons were formed in the Rhodopes), Mesozoic (when during the Alpine-Himalayan crimp the Sredna Gora mountain was formed), Cenozoic (when. The Regional geology of bulgaria and the Balkan Peninsula is the basis for all applied geosciences in this country thus representing the bridge from fundamental to applied research. The Department of Geotectonics and Regional geology at the Geological Institute of the Bulgarian Academy of Sciences is founded in 1962 by Academician Prof. Address: Department of Geotectonics and Regional Geology, Geological Institute, Bulgarian Academy of Sciences, Acad. Bonchev Street, Build.

75 Years Geological Institute Of BAS

Find 163 researchers and browse 12 departments, publications, full-texts, contact details and general information related to University of Mining and Geology | Bulgaria |. The geological formation of the Belogradchik Rocks is a result of millions of years of natural processes and various geological events. The rocks are primarily composed of sedimentary rock layers, which were formed during different geological periods. Around 230 million years ago, during the late Triassic period, the region where the. The Bulgarian Chamber of Mining and Geology supports the UN Global Compact and is an active member of the Bulgarian UN Network. Between 50 and 100% of the companies in Bulgaria with businesses in the respective branches of the industry are members of the Chamber. The Chamber members contribute up to 5% of the country's GDP, provide over. geology of bulgaria: A REVIEW [Foose, Richard M & Manheim, Frank] on . *FREE* shipping on qualifying offers. geology of bulgaria: A REVIEW. The Geological Institute is the only national complex geological organisation that systematically acquires knowledge on the geology of bulgaria, said also Prof. The 85th anniversary of Acad.

Bulgaria - East View Geospatial - Ivan Zagorchev was also celebrated. He is a respected scientist with worldwide recognition in the field of Earth sciences. Under the dome of the northern wing of Sofia University is situated a museum that throws light into the darkness of the distant geological ages. The Museum of Paleontology and Historical Geology houses in its collection and exposition more than 200 000 fossil specimens, rock samples, and geological maps of Bulgaria and the neighbouring territories. Sedmochislenitsi is a stratiform-stratabound Zn-Pb-Cu-Ag deposit hosted in Triassic carbonates in the NW of Bulgaria. The deposits have been compared to the Alpine-type Zn-Pb deposits of Raibl. Sofia University "St. Kliment Ohridski" Museum of Paleontology and Historical Geology is located within the 5th floor of the North Wing of the Main Building of the University. 15 Tzar Osvoboditel Blvd. За Геологическия институт. В продължение на повече от 70 години Геологическият институт е основно водещо звено в направлението "Науки за земята" при Българската академия на науките. The Rosen copper veins in southeastern Bulgaria are recognized for the first time as an iron oxide-copper-gold (IOCG) district. The veins are located in the East Srednogorie segment of the Carpathian-Balkan calc-alkaline volcano-plutonic arc and were formed during an end-stage interval of extreme slab rollback and intra-arc rifting, which gave rise farther east to seafloor spreading in the. Earth science mapping has been published by the former Committee of Geology and Mineral Resources and the Geological Institute 'Strashimir Dimitrov', Bulgarian Academy of Sciences (BAS). Several small-scale geological maps, some of recent origin and in English, are available, and a new 1:100,000 scale geological series in 86 sheets was completed in 1998. The Melnik Earth Pyramids (Bulgarian: Мелнишки пирамиди) are rock formations, known as hoodoos, situated at the foothills of the Pirin mountain range in south-western span an area of 17 km 2 near the town of Melnik, Blagoevgrad Province. Reaching a height of up to 100 m these sandstone pyramids are shaped in forms, resembling giant mushrooms, ancient towers and. Title: geology of bulgaria: a Review.

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The geology of bulgaria consists of two major structural features. The Rhodope Massif in southern Bulgaria is made up of Archean, Proterozoic and Cambrian rocks and is a sub-province of the Thracian-Anatolian polymetallic province. It has dropped down, faulted basins filled with Cenozoic sediments and volcanic rocks. The Review of Bulgarian Geological Society (BGS) is a scientific periodical which publishing starts in Its main purpose is to popularize the scientific achievements of Bulgarian and foreign geologists. The publishing is financed by the Bulgarian Geological Society by means of membership dues, sponsorship from BAS and other organizations and companies. The total volume of vitrified high-level waste (HLW) and of intermediate-level wastes containing significant amounts of long-lived alpha emitters, generated over the lifetime of Kozloduy Nuclear Power Plant (NPP), is estimated to be about 2,100 m Selection of a suitable formation to host a deep HLW repository in Bulgaria presents. The Proceedings in the Humanities and Social Sciences of the University of Mining and Geology "St. Ivan Rilski" is a scientific publication of the University of Mining and Geology "St. Ivan Rilski", with an editorial board, included in the National Reference List (NRL) of Contemporary Bulgarian Scientific Publications with Scientific Review maintained by the Minister of Education and. Geologically, Northern Bulgaria is within the ex panse of a platform structure, known as the Moe sian Plate (Atanasov, Bokov, 1983; Dabovski et al.



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