Geoloski Anali Balkanskog Poluostrva最新文献_第8页

Assessment of the discharge regime and water budget of Belo Vrelo (source of the Tolišnica River, central Serbia) Belo Vrelo(塞尔维亚中部Tolišnica河源头)的排放制度和水量预算评估

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1475093C

Marina Čokorilo-Ilić, Vesna Ristić-Vakanjac, Sibela Oudech, B. Vakanjac, D. Polomcic, Dragoljub Bajić

{"title":"Assessment of the discharge regime and water budget of Belo Vrelo (source of the Tolišnica River, central Serbia)","authors":"Marina Čokorilo-Ilić, Vesna Ristić-Vakanjac, Sibela Oudech, B. Vakanjac, D. Polomcic, Dragoljub Bajić","doi":"10.2298/GABP1475093C","DOIUrl":"https://doi.org/10.2298/GABP1475093C","url":null,"abstract":"A sufficiently long spring discharge regime monitoring data set allows for a large number of analyses, to better understand the process of transformation of precipitation into a discharge hydrograph. It is also possible to determine dynamic groundwater volumes in a karst spring catchment area, the water budget equation parameters and the like. It should be noted that a sufficiently long data set is deemed to be a contin- uous spring discharge time series of more than 30 years. Such time series are rare in Serbia. They are gener- ally much shorter (less than 15 years), and the respective catchment areas therefore fall into the \"ungauged\" category. In order to extend existing karst spring discharge time series, we developed a model whose outputs, apart from mean monthly spring discharges, include daily real evapotranspiration rates, catchment size and dynamic volume variation during the analytical period. So far the model has solely been used to assess the discharge regime and water budget of karst springs. The present paper aims to demonstrate that the model also yields good results in the case of springs that drain aquifers developed in marbles. Belo Vrelo (\"White Spring\", source of the Tolisnica River), which drains marbles and marbleized limestones and dolomites of Cemerno Mountain, was selected for the present case study.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"25 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125966217","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Thermomineral water of Nikoličevo Spa (Eastern Serbia) nikoli<s:1>埃沃温泉(东塞尔维亚)温泉水

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0701091D

P. Dokmanović, V. Dragišić, Slavko Spadijer

引用次数: 0

New dasycladales and microbiota from the lowermost Valanginian of the Mirdita zone Mirdita带最下端瓦兰吉尼亚期的新水系门和微生物群

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0566027R

R. Radoičić

{"title":"New dasycladales and microbiota from the lowermost Valanginian of the Mirdita zone","authors":"R. Radoičić","doi":"10.2298/GABP0566027R","DOIUrl":"https://doi.org/10.2298/GABP0566027R","url":null,"abstract":"A rich diversified algal microbiota is described from the lowermost Valanginian limestone reworked in the Upper Cretaceous elastics of the Metohija Cretaceous Unit (Mirdita Zone). Two new dasycladalean taxa are introduced: Zujovicella nov. gen. (type species Suppiluliumaella gocanini Radoicic, 1972) and Furcoporella vasilijesimici nov. sp. Microbiota of this bioclastic limestone (containing dominantly corals and other metazoan fragments) consists of algae, microbial epiliths, microproblematica, foraminifera, calcispongie and a few calpionellids of the Calpionellopsis Zone - Calpionellopsis oblonga (Cadisch), Remaniella cadischiana (Colom), Tinntinopsella carpathica (Murgeanu & Filipescu). Besides the new taxa dasycladales also associated are: Salpingoporella pygmaea (Gumbel), Salpingoporella sp., Gyroporella lukicae Sokac & Velic, Neomerinae and several indetermined taxa. Lithocodium aggregatum (Elliott), other encrusting Lithocodioidea and different microbial epiliths are an important component of this microbiota association. Foraminiferal assemblage consists of: Coscinophragma cf. C. cribrosum (Reuss), Mohlerina basiliensh (Mohler), Nautiloculina bronnimanni Arnaud-Vanneau & Peybernes, Neotrocholina valdensis Reichel, Neo-trocholina sp. Placopsilina sp., Protopeneroplis trochangulata Septfontaine, Trocholina alpina (Leupold), Trocholina delphinensis Arnaud-Vanneau, Boisseau & Darsac, Trocholina sp., lituolids, miliolids and other small benthic taxa. The analyzed lowermost Valanginian limestone originated from the topmost sequence of the Tithonian-Neocomian cycle which ended as a consequence of the Main Cimmerian Events, which occerred, as in the Vardar zone, after the lowermost Valanginian. Cretaceous cycle (Mirdita Crtaceous Unit) begins in the Hauterivian.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"129417674","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 21

Do major Neogene hiatuses in the Ciscaucasian semi-enclosed basin (Eastern Paratethys, southwestern Russia) record eustatic falls? 顺高加索半封闭盆地(俄罗斯西南部的东帕拉提提斯)的主要新近纪断裂是否记录了上升的下降?

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1071001R

A. Ruban, M. Rogerson, H. M. Pedley

{"title":"Do major Neogene hiatuses in the Ciscaucasian semi-enclosed basin (Eastern Paratethys, southwestern Russia) record eustatic falls?","authors":"A. Ruban, M. Rogerson, H. M. Pedley","doi":"10.2298/GABP1071001R","DOIUrl":"https://doi.org/10.2298/GABP1071001R","url":null,"abstract":"Hiatuses in semi-enclosed basins can be caused by either eustatic falls or local tectonic uplifts. The Ciscaucasian basin is located in the south of European Russia. In the Neogene, it belonged to the Eastern Paratethys domain. On the basis of available stratigraphic data, four major hiatuses are traced in this basin as erosional surfaces or lengthy sedimentation breaks, namely the Tarkhanian, Middle/Upper Sarmatian, Sarmatian/Maeotian, and Kimmerian hiatuses. They are documented in most of the areas of the study basin. The three earlier hiatuses mark short-term and nearly isochronous, basinwide sedimentation breaks, whereas the latter hiatus is diachronous, embracing more than 2 myr. All reported hiatuses record the eustatic falls. Consequently, we argue that eustatic processes controlled sedimentation in the Ciscaucasian basin throughout the entire Neogene. This means the basin was connected to the open ocean throughout this period, with important consequences for our understanding of watermass history in the Mediterranean and Paratethyan basins further west and south.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"119 6","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"120823926","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 1

Crystallite size distribution of clay minerals from selected Serbian clay deposits 塞尔维亚粘土矿床中粘土矿物的晶粒尺寸分布

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0667109S

V. Šimić, P. Uhlík

引用次数: 12

The impact of geology on the migration of fluorides in mineral waters of the Bukulja and Brajkovac pluton area) Serbia 地质对塞尔维亚布库尔贾和布拉伊科瓦茨岩体地区矿泉水中氟化物迁移的影响

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1273109P

P. Papic, Ilija Djokovic, J. Stojković, V. Jović, Goran Marinkovic, Z. Nikić

{"title":"The impact of geology on the migration of fluorides in mineral waters of the Bukulja and Brajkovac pluton area) Serbia","authors":"P. Papic, Ilija Djokovic, J. Stojković, V. Jović, Goran Marinkovic, Z. Nikić","doi":"10.2298/GABP1273109P","DOIUrl":"https://doi.org/10.2298/GABP1273109P","url":null,"abstract":"One of the hydrogeochemical parameters that classify groundwater as mineral water is the con- tent of fluoride ions. Their concentration is both important and limited for bottled mineral waters. Hydrochemical research of mineral waters in the surrounding area of Bukulja and Brajkovac pluton, in cen- tral Serbia, was conducted in order to define the chemical composition and genesis of these waters. They are carbonated waters, with content of fluoride ranging from 0.2 up to 6.6 mg/L. Since hydrochemical analyses showed variations in the major water chemistry it was obvious that, apart from hydrochemical research, some explorations of the structure of the regional ter:rain would be inevitable. For these pulposes, some additional geological research was performed, creating an adequate basis for the interpretation of the genesis of these carbonated mineral waters. The results confirmed the significance of the application of hydrochemical meth- ods in the research of mineral waters. The work tended to emphasize that \"technological treatment\" for decreasing the consentration of fluoride in mineral waters occurs in nature, indicating the existence of natu- ral defluoridization.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"2 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123203727","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Petrology of the Garnet Amphibolites from the Tejići Village - Povlen Mt., Western Serbia 塞尔维亚西部Tejići Povlen山村石榴石角闪岩的岩石学研究

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0264187S

Danica Srećković-Batoćanin, D. Milovanović, K. Balogh

引用次数: 4

PETROLOGY AND P‡T CONDITION OF WHITE MICA‡CHLORITE SCHISTS FROM VLASINA SERIES (SURDULICA, SE SERBIA) 塞尔维亚南部苏杜利卡地区vlasina系列白色云母绿泥石片岩的岩石学及沉积条件

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0264199V

J. N. Vaskovic

{"title":"PETROLOGY AND P‡T CONDITION OF WHITE MICA‡CHLORITE SCHISTS FROM VLASINA SERIES (SURDULICA, SE SERBIA)","authors":"J. N. Vaskovic","doi":"10.2298/GABP0264199V","DOIUrl":"https://doi.org/10.2298/GABP0264199V","url":null,"abstract":"This paper reports structural, textural, petrological and metamorphic data from Vlasina Series of greenschsts rocks (as part of the Upper Complex of the Serbo‡Macedonian Massif) within which group of white mica‡chlorite schist are extensively developed. This group of rocks made the ground of series in which various types of green rocks appear as a lenses and small irregular mass, rarely as dykes. Other features, that characterize these rocks, are the common occurrence of albite and garnet (subordinate) porphyroblasts, as well as development of quartz segregation. Group of white mica‡chlorite schist makes about 75 vol. % of Series. Among them, according to mode and mineral composition, the following schist varieties are distinguished: albite‡white mica‡chlorite (±garnet), white mica‡chlorite (±garnet), albite‡white mica, sericite‡chlorite (±albite), graphite‡sericite as well as phyllites and calcshists. Their metamorphic evolution is characterized by the development of a metamorphic episode during Carboniferous ‡ c. 350‡330 Ma (Milovanovi} et al., 1988) of low to medium P and T. The mineral assemblages of first phase (low PT) is preserved as a very thin Si=S1 foliation included in albite porphyroblast or as small polygonal arcs of S1 in S2 foliation. Textural, mineralogical and petrological data indicate that original volcanoclastic‡sedimentary series was transformed during three phase of deformation and metamorphism in the temperature range from 320‡415°C, locally 450‡500°C and pressures 3 to 5 kbar.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"331 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115973488","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 5

Discrimination of tectonic dynamism, quiescence and third order relative sea level cycles of the Cauvery Basin, South India 南印度柯韦里盆地构造动力、静息和三级相对海平面旋回的辨析

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1576

M. Ramkumar

引用次数: 9

Extensional unroofing of the Veliki Jastrebac dome (Serbia) Veliki Jastrebac圆顶的伸展拆除(塞尔维亚)

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0701021M

M. Marovic, Ilija Djokovic, M. Toljić, D. Spahić, J. Milivojević

{"title":"Extensional unroofing of the Veliki Jastrebac dome (Serbia)","authors":"M. Marovic, Ilija Djokovic, M. Toljić, D. Spahić, J. Milivojević","doi":"10.2298/GABP0701021M","DOIUrl":"https://doi.org/10.2298/GABP0701021M","url":null,"abstract":"This paper presents the basic structural elements of the dome of Veliki Jastrebac, as well as the chronology and mechanisms of the deformational events responsible for its formation. It was determined that the dome of Veliki Jastrebac consists of two large sequences which are, in the vertical section, in the inverse position. The lower part is made of Late Cretaceous and Cretaceous-Palaeogene low-grade to medium-grade metamorphic rocks, which are intruded by Paleogene granitoid (probably the Vardar Zone), which are covered with a large overthrust consisting metamorphics of the Serbian-Macedonian Mass. The low-grade to medium-grade metamorphosed complex of Veliki Jastrebac, with the granitoid, represents a metamorphic core complex, ex- humed by mechanisms of extensional tectonics in the Paleogene. Apstrakt. U radu su prikazani osnovni elementi gra|e Velikojastreba~ke dome i hronologija i meha- nizmi deformacionih doga|aja odgovornih za weno formirawe. Utvr|eno je da domu izgra|uju dva krupna navla~no-naborna entiteta koja su, u vertikalnoj sukcesiji, u inversnom poloaju. Dole lee gorwo- kredne i kredno-paleogene nisko do sredwometamorfisane stene u koje je utisnut paleogeni granitoid (verovatno Vardarska zona), gore je kao krupna navlaka, kristalin Srpsko-makedonske mase. Nisko do sredwe metamorfisan kompleks Velikog Jastrepca sa granitoidom predstavqa metamorfni core com- plex, ekshumiran mehanizmima ekstenzione tektonike u paleogenu.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"24 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"124437205","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 21