New data on the geology of the archaeological site at Vinča (Belgrade, Serbia)

L. Rundić, S. Kneževič, V. Kuzmic, Petar Kuzmič
{"title":"New data on the geology of the archaeological site at Vinča (Belgrade, Serbia)","authors":"L. Rundić, S. Kneževič, V. Kuzmic, Petar Kuzmič","doi":"10.2298/GABP1273021R","DOIUrl":null,"url":null,"abstract":"Landslides threaten Vinca, a world famous archaeological site of Neolithic \n culture. For this reason, a field investigation and geologic-geotechnical \n research of the cores of seven exploration boreholes were carried out. Avery \n interesting structural setting was identified. The oldest stratigraphic unit \n consists of Middle Miocene Sarmatian sediments, which were discovered along \n the right bank of Danube River and within its riverbed about 300 m upstream \n from the archaeological site. These Sarmatian strata give evidence that the \n Danube River eroded the right bank. In addition, within its recent valley, \n there is a fault zone along which a block on the right bank was uplifted \n while a block on the left bank of the river that was subsided. All the \n boreholes passed through sediments of a previously unknown geological \n formation. It lies unconformably over Sarmatian strip marls and makes the \n base for Pleistocene loessoid sediments (approx. 10 m under the surface). \n These sediments were formed in a marsh-lake environment with a strong river \n influence. According to its superposition, the supposed age of this formation \n is the Plio-Pleistocene. Above the right bank of the Danube River, there are \n steep sections where Pleistocene swamp loessoid sediments were found. True \n loess deposits are not present here, but are in the hinterland of the right \n bank of the Danube River. The loess delluvium was deposited over the \n Pleistocene sediments. On the right bank of the Danube River, below the \n archaeological site, there are the anthropogenic water compacted sands that \n were previously incorrectly shown on geological maps as alluvial fans. \n [Projekat Ministarstva nauke Republike Srbije, br. 176015]","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"104 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"8","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geoloski Anali Balkanskog Poluostrva","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2298/GABP1273021R","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 8

Abstract

Landslides threaten Vinca, a world famous archaeological site of Neolithic culture. For this reason, a field investigation and geologic-geotechnical research of the cores of seven exploration boreholes were carried out. Avery interesting structural setting was identified. The oldest stratigraphic unit consists of Middle Miocene Sarmatian sediments, which were discovered along the right bank of Danube River and within its riverbed about 300 m upstream from the archaeological site. These Sarmatian strata give evidence that the Danube River eroded the right bank. In addition, within its recent valley, there is a fault zone along which a block on the right bank was uplifted while a block on the left bank of the river that was subsided. All the boreholes passed through sediments of a previously unknown geological formation. It lies unconformably over Sarmatian strip marls and makes the base for Pleistocene loessoid sediments (approx. 10 m under the surface). These sediments were formed in a marsh-lake environment with a strong river influence. According to its superposition, the supposed age of this formation is the Plio-Pleistocene. Above the right bank of the Danube River, there are steep sections where Pleistocene swamp loessoid sediments were found. True loess deposits are not present here, but are in the hinterland of the right bank of the Danube River. The loess delluvium was deposited over the Pleistocene sediments. On the right bank of the Danube River, below the archaeological site, there are the anthropogenic water compacted sands that were previously incorrectly shown on geological maps as alluvial fans. [Projekat Ministarstva nauke Republike Srbije, br. 176015]
塞尔维亚贝尔格莱德vin考古遗址的地质新数据
滑坡威胁着世界著名的新石器文化考古遗址长春。为此,对7个勘探钻孔的岩心进行了野外调查和地质-岩土工程研究。发现了非常有趣的结构设置。最古老的地层单元由中新世中期的萨尔马提亚沉积物组成,这些沉积物是在多瑙河右岸和距离考古遗址上游约300米的河床内发现的。这些萨尔马提亚地层证明多瑙河侵蚀了右岸。此外,在它最近的山谷里,有一个断层带,沿着这个断层带,右岸的一个地块凸起,而左岸的一个地块则下沉。所有的钻孔都穿过了一种以前未知的地质构造的沉积物。它不整合地位于萨尔马提亚条状泥灰岩上,是更新世黄土沉积物的基础。地表以下10米)。这些沉积物形成于河流强烈影响的沼泽湖环境。根据其叠加,推测该地层的年龄为上新世-更新世。在多瑙河右岸上方,有一些陡峭的地段,在那里发现了更新世沼泽黄土沉积物。这里不存在真正的黄土沉积,而是在多瑙河右岸腹地。黄土冲积层沉积在更新世沉积层之上。在多瑙河的右岸,考古遗址的下面,有人为的水压实砂,以前在地质图上错误地显示为冲积扇。[南斯拉夫]塞族共和国部长项目;176015]
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信