Geoloski Anali Balkanskog Poluostrva最新文献_第4页

Geological activity of humans represented in the world heritage sites of India, Italy, and Russia: Evidence of the anthropocene 以印度、意大利和俄罗斯为代表的世界遗产的人类地质活动:人类世的证据

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1677055A

M. K. Ansari, A. Moroni, D. Ruban, S. Zorina, A. Aloia, M. Ahmad, Natalia I. Panikarskaja, Ekaterina G. Radchenko, T. Singh, A. Statsenko

{"title":"Geological activity of humans represented in the world heritage sites of India, Italy, and Russia: Evidence of the anthropocene","authors":"M. K. Ansari, A. Moroni, D. Ruban, S. Zorina, A. Aloia, M. Ahmad, Natalia I. Panikarskaja, Ekaterina G. Radchenko, T. Singh, A. Statsenko","doi":"10.2298/GABP1677055A","DOIUrl":"https://doi.org/10.2298/GABP1677055A","url":null,"abstract":"The idea of the Anthropocene attracts attention of scientists, policy-makers, and broad public to the geological activity of humans and poses new important questions for the modern stratigraphy. The growth of the Anthropocene-related knowledge and its promotion can be based potentially on the UNESCO World Heritage Sites (WHS). On the one hand, many of these sites provide spectacular evidence of the human activity. On the other hand, these are remarkable tourist attractions. The WHSs of three heritage-rich countries, namely India, Italy, and Russia, have been assessed with regard to how these reflect the geological activity of humans. It is established that 65–90% of all WHSs in each country provide direct and indirect evidence of such an activity (artificial caves, terrace building, etc.), which appears to be enough for the general discussion of the idea of the Anthropocene. However, the distribution of the WHSs by their age allows focusing only on the “early” (before 1800 AD) start of the Anthropocene, which is not enough for full discussion of the lower limit of this unit. The examples considered in the present study imply that some WHSs alone provide very important pieces of the Anthropocene-related knowledge.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"9 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":"129892520","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: 4

Polymetallic Cu-Bi-(Pb-Zn-Co-Ag) mineralization of the Perin Potok locality near Bor, Serbia 塞尔维亚博尔附近Perin Potok地区多金属Cu-Bi-(Pb-Zn-Co-Ag)矿化

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1374039P

Aleksandar Pačevski, Kristina Šarić, V. Cvetkovic

{"title":"Polymetallic Cu-Bi-(Pb-Zn-Co-Ag) mineralization of the Perin Potok locality near Bor, Serbia","authors":"Aleksandar Pačevski, Kristina Šarić, V. Cvetkovic","doi":"10.2298/GABP1374039P","DOIUrl":"https://doi.org/10.2298/GABP1374039P","url":null,"abstract":"Complex polymetallic Cu-Bi-(Pb-Zn-Co-Ag) mineralization of the Perin Potok \u0000 locality occurs as disseminations and fine nests in \u0000 quartz-ankerite-(sericite) veins. The veins are located in metamorphic rocks \u0000 of the outer contact zone of the Variscan Gornjane Granitoid. The \u0000 mineralization consists of (in decreasing abundance): chalcopyrite, aikinite, \u0000 bismuth, galena, Ag,Bi-bearing tetrahedrite, sphalerite, cobaltite and an \u0000 unnamed Bi2Te mineral. All these phases form distinctive exsolutions and \u0000 intergrowths and they simultaneously precipitated from a very complex \u0000 hydrothermal fluid. Silver shows elevated contents in tetrahedrite (3.3-4.4 \u0000 wt. % Ag), galena (0.9-1.1 wt. % Ag) and in the unnamed Bi2Te mineral (0.9 \u0000 wt. % Ag). Such high Ag concentrations can imply that Ag minerals could be \u0000 also present. Minor amounts of rutile showing fine intergrowths with sericite \u0000 also occur in this paragenesis. This is W-bearing rutile that shows zoning \u0000 caused by up to 2.2 wt. % W. The studied mineralization is probably \u0000 genetically related to the Variscan Gornjane Granitoid, although the \u0000 possibility of derivation from the metamorphic basement should be also taken \u0000 into account. [Projekat Ministarstva nauke Republike Srbije, br. OI176016]","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"34 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":"131028302","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

Correlation of metabasic rocks from metamorphic soles of the Dinaridic and the Western Vardar zone ophiolites (Serbia): Three contrasting pressure-temperature-time paths 塞尔维亚Dinaridic与Vardar西部蛇绿岩变质底变质岩对比:三种不同的压力-温度-时间路径

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1273061S

Danica Srećković-Batoćanin, Nada Vasković, V. Matović, V. Gajić

{"title":"Correlation of metabasic rocks from metamorphic soles of the Dinaridic and the Western Vardar zone ophiolites (Serbia): Three contrasting pressure-temperature-time paths","authors":"Danica Srećković-Batoćanin, Nada Vasković, V. Matović, V. Gajić","doi":"10.2298/GABP1273061S","DOIUrl":"https://doi.org/10.2298/GABP1273061S","url":null,"abstract":"The field, petrological-mineralogical, geochemical and geochronological data \u0000 of the metamorphic sole rocks recorded beneath the Fruska Gora, Povlen \u0000 (Tejici), Stolovi and Banjska ophiolites in the Western Vardar Zone (WVZ) and \u0000 beneath the Zlatibor, Bistrica, Sjenicki Ozren and Brezovica ophiolites in \u0000 the Dinaridic ophiolite belt (DOB) in Serbia are compared. The focus has been \u0000 made on metabasic rocks formed in contact with the oceanic crust members: \u0000 cumulate gabbro and basalts of SSZ-type with E-MORB and OIB-signature and \u0000 more evolved tholeiitic basalts of MOR-affinity. Amphibole, the major phase \u0000 formed from the mafic sole components, depending on pressure-temperature \u0000 conditions exhibits compositional variations. According to mineral \u0000 assemblages, estimated P-T conditions and ages, the potential P-T paths are \u0000 given: high pressure - low temperature blueschist facies assemblage (7-9 kbar \u0000 and ~400°C and <300-350°C and 4-8 kbar), recorded only in the metamorphic \u0000 sole at the Fruska Gora (WVZ); high pressure - high temperature amphibolite \u0000 to granulite facies (8-10 kbar and >700-850°C), recorded in both domains, the \u0000 WVZ (Banjska) and the DOB (Bistrica, Sjenicki Ozren, Brezovica) and medium \u0000 pressure - medium temperature amphibolite facies assemblages (~3.5-7 kbar and \u0000 >350-650°C) recognized in the WZV (Tejici, Devovici) and the DOB (Zlatibor). \u0000 The peak metamorphic conditions point to depths of the oceanic lithosphere \u0000 detachment and its initial cooling at 10-30 km, but the ages and tectonic \u0000 setting of ophiolites remain poorly constrained. The summarized data may be \u0000 used as an important key in geodynamic evolution of the Mesozoic Tethyan \u0000 ophiolites. [Projekat Ministarstva nauke Republike Srbije, br. 176019 and br. \u0000 176016]","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"21 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":"130696003","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: 3

A storm event during the Maastrichtian in the Cauvery basin, South India 印度南部高韦里盆地马斯特里赫特时期的风暴事件

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0667035R

M. Ramkumar

引用次数: 5

Stratigraphy of the Krš Gradac section (SW Serbia) Krš Gradac剖面地层(塞尔维亚西南部)

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0970023R

R. Radoičić, D. Jovanović, M. Sudar

{"title":"Stratigraphy of the Krš Gradac section (SW Serbia)","authors":"R. Radoičić, D. Jovanović, M. Sudar","doi":"10.2298/GABP0970023R","DOIUrl":"https://doi.org/10.2298/GABP0970023R","url":null,"abstract":"In the Krs Gradac section (near to Sjenica, SW Serbia), a transition of a carbonate platform to basin facies are outcropped: Norian-lower Liassic shallow-water carbonates, middle Liassic-lower Dogger Ammonitico Rosso facies, and upper Bathonian into lowermost Cretaceous deep-water radiolarites in which the carbonate graded bed and mass flow layer are intercalated. The presence of a lower Dogger condensed sequence with the Bajocian protoglobigerinid event was hitherto not evidenced. It is documented that components of a graded bed are of extrabasinal (upper Triassic-lower Tithonian carbonate platform sediments) and intrabasinal (radiolarite, meta-andesite) origin, indicating a tectonic event not older than the early Tithonian. This tectonic event caused the fracturing of the carbonate platform, also partly basinal area. Consequently, the age of the graded bed is not older than the lower Tithonian. In the uppermost radiolaritic sediments in the Krs Gradac section (?middle-upper Tithonian-lowermost Cretaceous), a mass flow layer appears, which contains clasts of intrabasinal origin - different radiolarites, siliceous radiolarian argillites (some of which are unconsolidated with washed radiolarians and sponge spicules in a ferruginous sediment), sandstone grains, etc. The mass flow event is estimated as Berriasian. In the Krs Gradac radiolarite succession, the authors recognized two deep-water formations, an older one, upper Bathonian-lower Tithonian, between hardground (Dogger) and a graded bed, and a younger formation, which started with a graded bed. This formation, according to its stratigraphic position, corresponds to ?middle-upper Tithonian-lowermost Cretaceous.","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":"130962383","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: 10

Tertiary plutonic rocks of southern Serbia Vardar Zone as dimension stone 塞尔维亚南部Vardar带第三系深成岩作为次元岩

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1475085K

Lidja Kurešević, V. Šimić

引用次数: 0

A condensed succession at the Jurassic/Cretaceous transition in a shallowing basin on the eastern Russian Platform 俄罗斯台地东部浅水盆地侏罗纪/白垩纪过渡时期的浓缩演替

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0970001Z

S. Zorina, D. Ruban, Loon Tom A.J. Van

{"title":"A condensed succession at the Jurassic/Cretaceous transition in a shallowing basin on the eastern Russian Platform","authors":"S. Zorina, D. Ruban, Loon Tom A.J. Van","doi":"10.2298/GABP0970001Z","DOIUrl":"https://doi.org/10.2298/GABP0970001Z","url":null,"abstract":"The eastern periphery of the Russian Platform houses an exceptional record of the Jurassic/Cretaceous transition, which is represented by very thin sandstone beds. The presence of glaucony grains, phosphorite con- cretions and shark teeth indicates that the transitional sediments constitute a condensed succession, although the allochtonous origin of the glaucony grains in itself is not a reliable indicator. The combination with thin ammonite zones and a strongly diminished sedimentation rate, as low as ~0.05 cm/ka are, however, convinc- ing evidence. The Jurassic/Cretaceous transitional deposits accumulated in a basin the depth of which decreased simultaneously with a global eustatic sea-level fall. This coincidence suggests that condensed successions may form in shallowing environments, which contradicts the sequence-stratigraphic concept. Considering the charac- ter of the sediments under study, it appears that both stratigraphic and taphonomic condensation patterns occur in this part of the eastern Russian Platform. Apstrakt. Isto~ni obod Ruske Platforme pokazuje izuzetan podatak o jursko-krednom prelazu, koji je predstavqen veoma tankim slojevima pe{~ara. Prisustvo glaukonitskih zrna, fosfornih konkrecija i zubi ajkula ukazuju da prelazni sedimenti izgra|uju kondenzovanu sukcesiju i ako alohtono poreklo glaukonitskih zrna nije uvek pouzdan pokazateq. Kombinacija uskih amonitskih zona i jako smawewe brzine sedimentacije od ~0.05 cm/ka su svakako ubedqiv dokaz. Prelazni jursko-kredni sedimenti depono- vani su u basen ~ija se dubina istovremeno pove}ava sa padom eustati~kog nivoa svetskog mora. Ova koin- cidencija ukazuje da se kondenzovane sukcesije mogu formirati u plitkim sredinama, a koja je u suprotnos- ti sa konceptom sekventne stratigrafije. Razmatraju}i prou~avani karakter sedimenata, proizilazi da su se i stratigrafska i tafonomska kondenzacija de{avale u ovom delu isto~ne Ruske Platforme.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"72 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":"123163129","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

Trans-border (north-east Serbia/north-west Bulgaria) correlations of the Jurassic lithostratigraphic units 侏罗纪岩石地层单位的跨界(塞尔维亚东北部/保加利亚西北部)对比

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1172001T

P. Tchoumatchenco, Dragoman Rabrenović, Vladan J. Radulović, Nenad Malešević, Barbara V. Radulović

{"title":"Trans-border (north-east Serbia/north-west Bulgaria) correlations of the Jurassic lithostratigraphic units","authors":"P. Tchoumatchenco, Dragoman Rabrenović, Vladan J. Radulović, Nenad Malešević, Barbara V. Radulović","doi":"10.2298/GABP1172001T","DOIUrl":"https://doi.org/10.2298/GABP1172001T","url":null,"abstract":"Herein, correlations of the Jurassic sediments from NE Serbia with those of \u0000 NW Bulgaria are made. The following Jurassic palaeogeographic units: the \u0000 Eastern Getic, the Infra-Getic and the Moesian Platform are included in the \u0000 study. The East Getic was studied in the outcrops near Rgotina, where the \u0000 sedimentation started in the Hettangian and continued during the \u0000 Callovian-Late Jurassic and is represented by platform carbonates. The \u0000 Infra-Getic is documented by the sections of Dobra (Pesaca) and the \u0000 allochtonous sediments near the Stubik. Very important for the Infra-Getic \u0000 are the Late Jurassic volcano-sedimentary deposits of the Vratarnica Series, \u0000 which crop out near Vratarnica Village. The Jurassic Moesian platform was \u0000 studied in the sections near D. Milanovac and Novo Korito (Serbia) and in \u0000 their prolongation in NW Bulgaria into the Gornobelotintsi palaeograben. Very \u0000 important are the correlation in the region of Vrska Cuka (Serbia) and \u0000 Vrashka Chuka (Bulgaria) - Rabisha Village (Magura Cave). A revision of the \u0000 Jurassic sediments on the Vidin palaeohorst, which were studied in the \u0000 Belogradchik palaeohorst, Gorno-Belotintsi palaeograben, Belimel palaeohorst \u0000 and the Mihaylovgrad palaeograben, is made. The sedimentation on the Vidin \u0000 palaeohorst started during different parts of the Middle Jurassic, and in the \u0000 Mihaylovgrad palaeograben during the Hettangian (Lower Jurassic) where the \u0000 sediments were deposited in relatively deeper water conditions. To south, the \u0000 relatively shallow water sediments deposited on the Jurassic Vratsa \u0000 palaeohorst on the southern board of the Mihaylovgrad palaeograben are \u0000 described.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"3 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":"123391956","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: 6

Characteristic groundwater level regimes in the capture zones of radial collector wells and importance of identification (Case study of Belgrade Groundwater Source) 径向集水井捕获区地下水位特征及其识别的重要性(以贝尔格莱德地下水源为例)

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1677043B

Djordjije Bozovic, D. Polomcic, Dragoljub Bajić

引用次数: 1

Note on the first fossil remains of a whale from Northern Bosnia 在波斯尼亚北部发现的第一块鲸鱼化石

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1071127S

I. Stefanović

引用次数: 1