立陶宛西北部Šventoji-Būtingė沿海地区古切口的地球物理研究

Pub Date : 2013-12-11 DOI:10.5200/BALTICA.2013.26.21
D. Gerok, A. Bitinas
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引用次数: 1

摘要

古切口(古隧道、隧道谷、隐谷等)是斯堪的纳维亚大陆冰盖覆盖的亚第四纪地表最显著的特征。斯堪的纳维亚结晶基岩地区是个例外。从科学和实践的角度来看,古切口都是第四纪地质学的研究对象,以前已经沿着立陶宛沿海地区利用重力和瞬变电磁方法绘制了切口图,并辅以传统钻探。本文提出了立陶宛西北部Sventoji-Būtingė沿海地区古切口的高分辨率识别方法。已经测试了几种地球物理方法,包括浅层地震反射剖面、电断层成像和探地雷达。浅层地震反射和电层析成像的结合为高分辨率勘探提供了最佳的勘探策略
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Geophysical study of palaeo-incisions in the Šventoji-Būtingė coastal ar ea, north-west Lithuania
Palaeo-incisions (palaeo-tunnels, tunnel valleys, buried valleys, etc.) comprise the most prominent features in the sub-Quaternary surface covered by the Scandinavian continental ice sheets. An exception is the Scandinavian crystalline bedrock region. Palaeo-incisions are objects of Quaternary geology both from scientific and practical point of view and have been previously mapped along the Lithuanian coastal area using gravimetric and transient electromagnetic methods, complemented by traditional drilling. This paper presents an approach for high-resolution identification of the palaeo-incisions in the Sventoji-Būtingė coastal area of north-western Lithuania. Several geophysical methods have been tested, including shallow seismic reflection profiling, electrical tomography and ground-penetrating radar. A combination of shallow seismic reflection and electrical tomography profiling provides an optimal survey strategy for high-resolution investigations of
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