Geoloski Anali Balkanskog Poluostrva最新文献_第10页

Some species of the Genus Hemicytheria Pokorny (Ostracoda, Crustacea) from the Upper Miocene of Serbia 标题塞尔维亚中新世上部的半壳虫属(介形虫目，甲壳纲)若干种

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0264137R

L. Rundić

引用次数: 5

Late Barremian-Early Aptian Urgonian Limestones from the south-eastern Kučaj Mountains (Carpatho-Balkanides, Eastern Serbia) 库<s:1>阿伊山脉东南部(喀尔巴阡山脉-巴尔干山脉，塞尔维亚东部)晚巴雷米亚-早阿普提亚-乌尔哥尼亚石灰石

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0869013S

M. Sudar, D. Jovanović, A. Maran, S. Polavder

引用次数: 21

The copper deposits of Bor, eastern Serbia: Geology and origin of the deposits 塞尔维亚东部博尔铜矿床:地质和矿床成因

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1475059A

Ivana S Antonijević, P. Mijatovic

{"title":"The copper deposits of Bor, eastern Serbia: Geology and origin of the deposits","authors":"Ivana S Antonijević, P. Mijatovic","doi":"10.2298/GABP1475059A","DOIUrl":"https://doi.org/10.2298/GABP1475059A","url":null,"abstract":"The copper deposits of Bor, volcanic activities in the area and relationship \u0000 of minerals through time are presented by formations within the \u0000 Cenomanian-Turonian range. Geology and age of the deposits are given in the \u0000 geological-time order based on superposition of the Timok mineral-ore \u0000 Formation and the underlying (Cenomanian) and fossiliferous overlying \u0000 (Senonian) strata. The concept of dating Bor deposits the Turonian is \u0000 discussed in this context. Bor deposits lie between the Cenomanian Krivelj \u0000 Formation and the Senonian epiclastic Metovnica Formation. Embedded between \u0000 the two formations is the Timok volcanogenic Formation. Described in this \u0000 paper are principal members of the Timok Formation strata: volcanogenic and \u0000 subvolcanogenic- intrusive rocks, a zone of hydrothermally altered rocks and \u0000 main types of the Bor ore deposits: (a) Deposits of massive sulphide coppers; \u0000 (b) Vein and stockwork-disseminated type of mineralisation; (c) Porphyry \u0000 mineralisation; and (d) Reworked ore-clasts of copper sulphides of the Novo \u0000 Okno deposit. Identified deposits, according to the Bor Geological Service \u0000 records and published works, are systematized and summarized into three \u0000 geographic units: (1) Group of deposits Severozapad (Brezanik); (2) Central \u0000 Bor Deposits (Tilva Ros, Coka Dulkan, Tilva Mika, Borska Reka, and Veliki \u0000 Krivelj) and many ore bodies; (3) Copper deposits Jugoistok (ore bodies X and \u0000 J) and olistostrome deposit Novo Okno. Information given in this paper, the \u0000 discussion on relative geologic age of the Bor deposit’s floor and roof in \u0000 particular, support our concept that the process ceased before the Upper \u0000 Turonian, and that age of the primary copper mineralization is Turonian.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"43 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":"133398435","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

Involutina farinacciae Bronnimann & Koehn-Zaninetti 1969, a marker for the Middle Liassic in basinal and some platform facies of Mediterranean and near east areas: The discussion concerning the paleogeography of Montenegro-Albania border region (the Scutari-Pec lineament) Involutina farinacciae Bronnimann & Koehn-Zaninetti 1969，地中海和近东地区盆地和台地相的中叠世标志——关于黑山-阿尔巴尼亚边界地区(scutarii - pec)古地理的讨论

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP1172047R

R. Radoičić, D. Jovanović

{"title":"Involutina farinacciae Bronnimann & Koehn-Zaninetti 1969, a marker for the Middle Liassic in basinal and some platform facies of Mediterranean and near east areas: The discussion concerning the paleogeography of Montenegro-Albania border region (the Scutari-Pec lineament)","authors":"R. Radoičić, D. Jovanović","doi":"10.2298/GABP1172047R","DOIUrl":"https://doi.org/10.2298/GABP1172047R","url":null,"abstract":"Foraminiferal species Involutina farinacciae BRONNIMANN & KOEHN-ZANINETTI, is \u0000 a marker of Middle Liassic basinal and transitional platform bassin facies \u0000 widely distributed in Mediterranean area (Umbria-Marche, Pindos, Budva, \u0000 Sicilia and the Inner Dinarides basin), also in Iraqi Kurdistan (“Avroman” \u0000 Basin). In the Dinaric Carbonate Platform (DCP) it indicates intramarginal \u0000 and intraplatform depressions. Paleogeography of the Montenegro-Albania \u0000 border area formed by the inherited prealpine paleogeographic scenario that \u0000 resulted in a different arrangement of the paleogeographic units westward and \u0000 eastward of the paleostructure (Scutari-Pec Lineament) which controlled the \u0000 geological history of the region. This transverse paleostructure was a) \u0000 coincident with the paleogeographic front of the DCP, and b) the westward \u0000 limit of the overtrusted Mirdita Zone. The difference in the paleogeographic \u0000 features in the prolongation from the DCP througout Albania, controlled by \u0000 paleostructure, are the source of seizmicity, rotation and deviation (SE to \u0000 NW, into NE) of the Complex Mirdita Zone.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"28 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":"130417012","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

Linoporella buseri Radoičić, 1975, revisited: A Liassic dasycladalean alga from the Dinarides and continental Italy Linoporella buseri radoi<e:1>， 1975，重游:一种来自Dinarides和意大利大陆的晚纪浅基藻

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0970061R

R. Radoičić, A. Conrad, N. Carras

引用次数: 3

Pollen analyses of Pleistocene hyaena coprolites from Montenegro and Serbia 黑山和塞尔维亚更新世鬣狗粪化石的花粉分析

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0701073A

J. Argant, V. Dimitrijević

引用次数: 22

Gross Martin: Mittelmiozäne Ostracoden aus dem Wiener Becken (Badenium/Sarmatium, Österreich)/Middle Miocene Ostracods from the Vienna Basin (Badenian/Sarmatian, Austria): Verlag der Österreichischen 格罗斯·马丁:来自维也纳盆地的中部米斯特兰牛肉帝国(奥地利的贝金尼姆/沙马塔特姆)/奥地利维也纳盆地Ostracods

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0667123R

Ljupko Rundić

引用次数: 1

Neomeris mokragorensis sp. nov. (Calcareous alga, Dasycladales) from the Cretaceous of Serbia, Montenegro and the Northern Calcareous Alps, (Gosau Group, Austria) Neomeris mokragorensis sp. 11 .(石灰质藻类，Dasycladales)来自塞尔维亚、黑山和北石灰质阿尔卑斯山的白垩纪，(Gosau Group，奥地利)

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0701039R

R. Radoičić, F. Schlagintweit

引用次数: 10

Stratigraphy and lithology of the loess deposits in eastern Srem, Serbia 塞尔维亚斯雷姆东部黄土地层与岩性研究

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0566021N

D. Nenadić, V. Šimić

引用次数: 1

Late Miocene ostracodes of Serbia: morphologic and palaeoenvironmental considerations 塞尔维亚晚中新世介形类:形态和古环境的考虑

Geoloski Anali Balkanskog Poluostrva Pub Date : 1900-01-01 DOI: 10.2298/GABP0667089R

L. Rundić

{"title":"Late Miocene ostracodes of Serbia: morphologic and palaeoenvironmental considerations","authors":"L. Rundić","doi":"10.2298/GABP0667089R","DOIUrl":"https://doi.org/10.2298/GABP0667089R","url":null,"abstract":"About 11.5 million years ago, a tectonic uplift of the Eastern and Western Carpathians separated the Pannonian Basin from the rest of the Paratethys. This orogenesis event caused an unconformity between the Sarmatian brackish sediments and the Pannonian lake-sea deposits. More than 6 Ma later, in these parts of the Paratethys, changes in the geographic framework, hydrological conditions and brackish - caspibrackish water chemistry led to the disappearance of restricted marine forms of life. A few euryhaline and marginal marine species survived this environmental change. Among the ostracodes, some originally freshwater taxa, such as Candoninae, entered the lake-sea. Many lineages show gradual morphological changes. The older, low diversi- ty ostracode fauna from the Lower Pannonian dispersed to the endemic species and genera during the Upper Pannonian. This interval is assigned as the \"bloom time\" for many ostracodes, both qualitatively and quantita- tively. This time sequence is the last appearances of genera such as Aurila, Cytheridea, Propontoniella, etc. and simultaneously, the first appearances for many new genera, such as Zalanyiella, Serbiella, Camptocypria, Sinegubiella etc. During the Pontian, migration processes were present. Therefore, it can be supposed that many eastern Paratethyan forms have Pannonian origin.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"123 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":"127234273","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: 18