Annales g?ologiques de la Peninsule balkanique最新文献_第3页

A hundred years of Milutin Milankovic's climate change theory-geological implications 米卢廷·米兰科维奇的百年气候变化理论——地质意义

Annales g?ologiques de la Peninsule balkanique Pub Date : 1900-01-01 DOI: 10.2298/gabp201125011r

D. Radivojević

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New data on maastrichtian fishes of the ‘Haţeg Island’ 关于“Haţeg岛”马斯特里赫特鱼的新数据

Annales g?ologiques de la Peninsule balkanique Pub Date : 1900-01-01 DOI: 10.2298/gabp220424001t

Nicolae Trif, V. Codrea

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Microfacies and biostratigraphy of an Upper Triassic Dachstein limestone fore-reef block in the Jurassic Sirogojno carbonate-clastic Mélange (Zlatibor Mt., SW Serbia) 塞尔维亚Zlatibor山侏罗系Sirogojno碳酸盐岩-碎屑岩m<s:1> lange上三叠统Dachstein灰岩前礁块微相及生物地层学

Annales g?ologiques de la Peninsule balkanique Pub Date : 1900-01-01 DOI: 10.2298/gabp210518003z

Oliver Zöhrer, Gawlick Hans-Jürgen, George Pleș, M. Sudar, D. Jovanović

{"title":"Microfacies and biostratigraphy of an Upper Triassic Dachstein limestone fore-reef block in the Jurassic Sirogojno carbonate-clastic Mélange (Zlatibor Mt., SW Serbia)","authors":"Oliver Zöhrer, Gawlick Hans-Jürgen, George Pleș, M. Sudar, D. Jovanović","doi":"10.2298/gabp210518003z","DOIUrl":"https://doi.org/10.2298/gabp210518003z","url":null,"abstract":"In the late Middle to early Late Jurassic carbonate-clastic Sirogojno Melange in the Zlatibor Mountain there is one roughly 35 m thick overturned block with an intact Late Triassic fore-reefal Dachstein Limestone succession studied for its biostratigraphic age, content and microfacies characteristics. The succession starts with coarse-grained rudstones followed by meter-sized reefal blocks intercalated in partly layered resedimented grainstones and packstones with abundant reef-building organisms like calcareous sponges, corals and encrusting organisms. Inside this part of the succession open-marine influenced layers are rare. The succession continues with a partly turbiditic sequence and chaotic rudstones, densely packed with reef-derived material like broken reefbuilding organisms and shallow-water material like gastropods, bivalves and foraminifers. Grainstones with clear open-marine influence (e.g., thin-shelled bivalves, crinoids, conodonts) appear in between those rudstones, in cases lumachelle layers be composed of halobiids were deposited. To the end of the succession some layers show turbiditic bedding with mixed shallow-water and deep-marine grains and organisms, i.e. filaments and crinoids. On base of conodonts, foraminifers, calcareous algae, holothurians and halobiids throughout the whole studied succession, a middle Norian (Alaunian) to Rhae tian 1, most probably a late Norian (Sevatian) age can be assigned to this fore-reefal Dachstein Limestone succession, with a similar sedimentation pattern like Late Triassic Dachstein fore-reef limestone facies, e.g., in the Northern Calcareous Alps or the eastern Southern Alps. The study of this block in the Sirogojno Melange closes an important gap in knowledge about the extent, facies and stratigraphy of the Dachstein Carbonate Platform evolution in the Dinarides.","PeriodicalId":378337,"journal":{"name":"Annales g?ologiques de la Peninsule balkanique","volume":"31 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":"123414151","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}

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A first attempt at a provenance study in the Jadar block (Serbia) by means of U-Pb zircon geochronology 用U-Pb锆石年代学方法研究塞尔维亚Jadar地块物源的首次尝试

Annales g?ologiques de la Peninsule balkanique Pub Date : 1900-01-01 DOI: 10.2298/gabp230303005l

Georg Löwe, D. Prelević, K. Ustaszewski

{"title":"A first attempt at a provenance study in the Jadar block (Serbia) by means of U-Pb zircon geochronology","authors":"Georg Löwe, D. Prelević, K. Ustaszewski","doi":"10.2298/gabp230303005l","DOIUrl":"https://doi.org/10.2298/gabp230303005l","url":null,"abstract":"U-Pb geochronology of zircon grains retrieved from magmatic rocks intruding\u0000 the Jadar block terrane in the central Balkans is used here to add new\u0000 constraints on the terrane accretion processes and the provenance of crustal\u0000 sources of this potentially exotic crustal block. Using an unorthodox\u0000 approach, we analyzed zircons extracted from the products of Cenozoic (Cer\u0000 and Boranja granitoid massifs) and Triassic magmatism (Bobija andesitic tuff\u0000 - Pietra Verde). In fourteen samples of granites and epiclastites, we\u0000 analyzed about 600 grains, and of these, about 30-40% were derived from the\u0000 basement and were used further for the geological interpretation. Most\u0000 samples show a similar Precambrian and Paleozoic age spectrum, including\u0000 ubiquitous Neoproterozoic and well-defined Silurian-Ordovician populations.\u0000 Only a few older zircons are present, composing minor populations at c. 1.2\u0000 Ga and 3.2 Ga. The younger zircons represent a ubiquitous Triassic\u0000 population that is the strongest in all samples. This age population is most\u0000 likely associated with local Permo-Triassic magmatism generated due to the\u0000 opening of the Neotethys. In contrast to the magmatic rocks of Boranja and\u0000 Bobija, the zircon age spectrum of the Cer polyphase pluton shows a strong\u0000 Carboniferous peak, indicating a potentially important link to the Variscan\u0000 margin of Eurasia. This supports opposing interpretations that either this\u0000 part of the Jadar block terrane represents a southern continuation of the\u0000 ?Bukkium? and Sana-Una terranes comprising displaced fragments of the\u0000 southern European Variscan foreland, or, more likely, that it has an Adria\u0000 affinity and that these zircons are derived from Cretaceous sediments of the\u0000 Sava Zone, i.e., the suture that separates European and Adriatic domains,\u0000 which were assimilated during the intrusion of the Cer granitic magmas.","PeriodicalId":378337,"journal":{"name":"Annales g?ologiques de la Peninsule balkanique","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":"130491864","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}

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Stratigraphy revision of upper Badenian of Rakovica stream near Belgrade (Central Paratethys, Serbia) 塞尔维亚中部Paratethys地区贝尔格莱德附近Rakovica河上巴登尼亚期地层修正

Annales g?ologiques de la Peninsule balkanique Pub Date : 1900-01-01 DOI: 10.2298/gabp200213005j

G. Jovanović, S. Vrabac, S. Ćorić

{"title":"Stratigraphy revision of upper Badenian of Rakovica stream near Belgrade (Central Paratethys, Serbia)","authors":"G. Jovanović, S. Vrabac, S. Ćorić","doi":"10.2298/gabp200213005j","DOIUrl":"https://doi.org/10.2298/gabp200213005j","url":null,"abstract":"Belgrade area is a region of high paleobiodiversity, being ranked among the best known in Serbia. The prominent position among a number of Middle Miocene (Badenian) fossiliferous sites in the vicinity of Belgrade (southern Pannonian Basin, Central Paratethys) are occupied with sediments of Rakovica stream, also known as ?Rakovica sands?. Here, the integrated evidence based on new fossil findings of calcareous nannoplankton, foraminifera and molluscs assemblages, allows the stratigraphic revision of the clastic facies of the Rakovica succession. Based on the studies of lithological composition, high paleodiversity molluscs fauna and local palaeogeographical setting, it can be concluded with reasonable certainty that deposits of Rakovica stream entitled ?Rakovica sand? represents a sandstone of the shallow marine (littoral) environment during Lower Badenian time. Large benthic foraminifera Ammonia viennensis (d?ORBigny), and Borelis haueri (d?ORBigny) as well as zone marker nn5 Sphaenolithus heteromorphus defLandRe correspond to this biostratigraphic level. during the late early Miocene and Middle Miocene (Badenian), the climate in the Central Paratehys was mainly subtropical. This is supported at its southern margin by the presence of thermophilous mollusc taxa, as well as the Conidae, Strombidae, Xenophoridae, Pleurotomidae, Turridae, Muricidae, etc. Consequently, the investigated deposit can be ascribed to the early Badenian which biostratigraphically corresponds to the nn5 nannozone by correlation with successions in theirs type-areas to the Central Paratethys, and defines preciously the time of the marine transgression in this area.","PeriodicalId":378337,"journal":{"name":"Annales g?ologiques de la Peninsule balkanique","volume":"341 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":"115270026","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}

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The revision of quaternary stratigraphy of the Zrenjanin artesian well borehole profile (Banat, Vojvodina, Serbia) 塞尔维亚伏伊伏丁那省巴纳特Zrenjanin自流井井剖面第四纪地层订正

Annales g?ologiques de la Peninsule balkanique Pub Date : 1900-01-01 DOI: 10.2298/gabp210306007g

T. Gaudenyi, D. Nenadić, M. Jovanović, P. Stejic

{"title":"The revision of quaternary stratigraphy of the Zrenjanin artesian well borehole profile (Banat, Vojvodina, Serbia)","authors":"T. Gaudenyi, D. Nenadić, M. Jovanović, P. Stejic","doi":"10.2298/gabp210306007g","DOIUrl":"https://doi.org/10.2298/gabp210306007g","url":null,"abstract":"The geological analysis of artesian borehole material from Sombor, Subotica,\u0000 and Zrenjanin, was in the first campaign of detailed stratigraphic studies\u0000 of Vojvodina in 1892-1895. The results of Quaternary stratigraphy from\u0000 Zrenjanin were published by HalavAts m ore than a decade later (1914). The\u0000 significance of the Zrenjanin, Sombor, and Subotica artesian well profiles\u0000 for more than a century is considered the representative local profiles for\u0000 the Quaternary stratigraphy of Vojvodina recognized by Serbian (Yugoslavian)\u0000 and Hungarian geologists. Significant changes were after the taxonomical\u0000 revision of molluscan material and its stratigraphic context, which was done\u0000 through the excellent work of Krolopp in the 1970-ies. Unfortunately, the\u0000 mentioned changes were not applied in the studies during the geological\u0000 surveying of former Yugoslavia. The developments in Quaternary geology,\u0000 changes in the Quater nary chronostratigraphic scale, and the results shown\u0000 by this paper enable the Lower Pleistocene fluvial deposits to be defined as\u0000 the Pleistocene Corbicula beds, the Viviparus boeckhi Horizon. The Lower\u0000 Pleistocene at Zrenjanin was documented from 234.54 to 58.36 m depth. The\u0000 interval between 234.54 and 208.50 m comprises the Upper Paludina -\u0000 Viviparus vucotinovici zone, while the Viviparus boeckhi Horizons were\u0000 identified between 135.18 m and 58.36 m. The interval between 58.36 m and\u0000 37.75 m is defined as Pleistocene (Lower- and Middle Pleistocene) based on\u0000 sedimentological and the molluscan record. The interval from 37.75 m to\u0000 21.67 m depth was identified as Middle Pleistocene, according to its\u0000 lithology and the paleontological material. The fluvial sediments? 21.69 m\u0000 and 7.31 m depths cannot be determined according to the faunistic data; we\u0000 can only consider them as Pleistocene age. The Holocene sediment and soil\u0000 horizons ascend to a 2.90 m depth.","PeriodicalId":378337,"journal":{"name":"Annales g?ologiques de la Peninsule balkanique","volume":"7 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":"125373119","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

Early-Middle Jurassic stepwise deepening in the transitional facies belt between the Adriatic Carbonte Platform Basement and Neo-Tethys open shelf in northeastern Montenegro evidenced by new ammonoid data from the early Late Pliensbachian (Lavinianum Zone) 晚Pliensbachian早期(Lavinianum带)新氨样资料证明黑山东北部早-中侏罗统亚得里亚海碳酸盐岩台地基底与新特提斯陆架过渡相带逐步加深

Annales g?ologiques de la Peninsule balkanique Pub Date : 1900-01-01 DOI: 10.2298/GABP201230001D

M. Djakovic, H. Gawlick, M. Sudar

{"title":"Early-Middle Jurassic stepwise deepening in the transitional facies belt between the Adriatic Carbonte Platform Basement and Neo-Tethys open shelf in northeastern Montenegro evidenced by new ammonoid data from the early Late Pliensbachian (Lavinianum Zone)","authors":"M. Djakovic, H. Gawlick, M. Sudar","doi":"10.2298/GABP201230001D","DOIUrl":"https://doi.org/10.2298/GABP201230001D","url":null,"abstract":"New ammonoid data prove an early Late Pliensbachian deepening event above the ?Late Hettangian-Sinemurian shallow-subtidal gray-reddish micro-oncoidal-foraminifera grainstone facies and the ?early Pliensbachian deeper-marine micro-oncoidal-crinoidal-ammonoid wacke- to packstone facies. Based on the presence of Fuciniceras lavinianum (Fucini), Lytoceras ovimontanum Geyer and Arieticeratinae gen. indet. from a hardground above the deeper-water micro-oncoidal limestones in the Mihajlovici section (north - eastern Montenegro) a Late Pliensbachian to early Toarcian condensation horizon is proven. The Middle Toarcian ammonoid-bearing horizon also yielded species not known from previous studies: Calliphylloceras capitanii (cATuLLo), Harpoceras subplanatum (oPPeL) and Furloceras aff. chelussii (PAriScH & ViALe), also described in the present paper. These new data prove a stepwise deepening of the depositional area during the early and the Middle Jurassic reflected in detail in four sedimentary members: 1) ?Late Hettangian to Sine - murian/?earliest Pliensbachian open-marine shallow subtital micro-oncoidal limestones; 2) ?early to Late Pliensbachian open-marine condensed limestones with few micro-oncoids and more open-marine influence; 3) Toarcian open-marine condensed red limestones with hardgrounds; and 4) condensed red nodular Bositra Limestone. These four members are separated by hard - rounds representing stratigraphic gaps in deposition. The stepwise deepening during the early-Middle Jurassic follows the general trend of deposition as known in the whole Western Tethys realm above the Late Triassic Dachstein carbonate Platform.","PeriodicalId":378337,"journal":{"name":"Annales g?ologiques de la Peninsule balkanique","volume":"238 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":"115923626","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

Novel findings of late Cenomanian-Turonian Pachyophiid snakes, fishes and plants in the SE Bosnia-Herzegovina 波斯尼亚-黑塞哥维那东南部晚塞诺曼-土尔onian厚皮蛇类、鱼类和植物的新发现

Annales g?ologiques de la Peninsule balkanique Pub Date : 1900-01-01 DOI: 10.2298/gabp220406003d

D. Djuric, N. Djerić, U. Stojadinovic, Desa Djordjevic-Milutinovic, Miodrag Hrnjez Ljumo, Milan Denda

引用次数: 0

Tectono-sedimentary evolution of the NE dinarides margin: vestiges of the Adria-Europe convergence in cretaceous sedimentary formations of central Serbia 东向二叠纪边缘的构造-沉积演化:塞尔维亚中部白垩纪沉积地层中亚德里亚-欧洲辐合的遗迹

Annales g?ologiques de la Peninsule balkanique Pub Date : 1900-01-01 DOI: 10.2298/gabp230112001s

U. Stojadinovic, Nemanja Krstekanić

{"title":"Tectono-sedimentary evolution of the NE dinarides margin: vestiges of the Adria-Europe convergence in cretaceous sedimentary formations of central Serbia","authors":"U. Stojadinovic, Nemanja Krstekanić","doi":"10.2298/gabp230112001s","DOIUrl":"https://doi.org/10.2298/gabp230112001s","url":null,"abstract":"The Cretaceous sedimentation along the NE Dinarides margin occurred in basins\u0000 above the Europe-dipping Neotethyan Sava subduction zone positioned between\u0000 Adria- and Europe-derived continental units. The Cretaceous sedimentation on\u0000 the upper plate of the Sava subduction system took place in a fore-arc\u0000 basin, developed in frontal parts of the active European continental margin.\u0000 The Cretaceous sedimentation in the lower Adria plate domain of the Sava\u0000 subduction system includes sediments deposited in the basin developed over\u0000 the passive continental margin of the Internal Dinarides and the sediments\u0000 deposited in the Sava subduction trench. While the Cretaceous sedimentation\u0000 on the entire Adriatic continental margin was associated with an overall\u0000 contraction, which led to the progressive subsidence towards the end of the\u0000 Cretaceous, the fore-arc basin on the European continental margin displays\u0000 three depositional cycles during the Early Cretaceous-Cenomanian,\u0000 Turonian-Santonian, and Campanian-early Paleogene, reflecting three stages\u0000 of deformation, contraction, extension, and ultimately contraction again\u0000 during the Adria-Europe collision.","PeriodicalId":378337,"journal":{"name":"Annales g?ologiques de la Peninsule balkanique","volume":"311 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":"133773015","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

Hazardous substances in karst aquifer waters - one of the results of the operational monitoring of groundwater in Serbia 喀斯特含水层水中的有害物质——塞尔维亚地下水运行监测的结果之一

Annales g?ologiques de la Peninsule balkanique Pub Date : 1900-01-01 DOI: 10.2298/gabp201107010s

Z. Stevanović, Veljko Marinović, B. Petrović

{"title":"Hazardous substances in karst aquifer waters - one of the results of the operational monitoring of groundwater in Serbia","authors":"Z. Stevanović, Veljko Marinović, B. Petrović","doi":"10.2298/gabp201107010s","DOIUrl":"https://doi.org/10.2298/gabp201107010s","url":null,"abstract":"Hydrogeological survey of wider Majdanpek mining area in the Carpathian mountain arch of eastern Serbia, including open mine pits, tailings sites, and major karstic springs and caves has been undertaken in order to estimate environmental conditions in groundwater body (GWB) ?Krs?sever?, groundwater quality, and to investigate causes of their earlier indicated poor chemical status. Bearing in mind that Majdanpek copper mine field is directly bordering the karst aquifer and delineated GWB ?Krs?sever?, the two karst springs namely Valja Fundata and Kaludjerica were in situmeasured and sampled in high and low-water periods (spring 2019, late autumn 2019 and spring 2020). Sampling and analysis of groundwater were carried out under the frame of project ?Operational Monitoring of Groundwater of the Republic of Serbia?, established by the Ministry of Environmental Protection of Serbia. The field measurements of unstable chemical components and physical properties as well as laboratory analyses confirmed very poor and even hazardous water quality of both surveyed springs Valja Fundata and Kaludjerica. Registered concentrations of some ions, such as Fe2+, Mn2+, Ca2+, SO4 2?are high above maximal permitted level for potable water in Serbia. High turbidity rate also confirms impact of colloidal suspensions from the tailing which is located in karstic blind valley. Leakage of mine water passes through joints, open cavities and even large cave system Valja Fundata. Results of undertaken survey confirm that low-water period results with worse water quality and much higher concentration of hazardous substances than that characterized high-water season when infiltrated rainy water and/or melted snow dilute tailing?s wastewater. Strict application of environmental protection measures and de - sign/construction of the smaller water treatment facility at both surveyed springs should possibly mitigate the impacts of mining activities to karst groundwater and dependant ecosystem.","PeriodicalId":378337,"journal":{"name":"Annales g?ologiques de la Peninsule balkanique","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":"128458497","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