A pilot study of the dependence of radon concentration on the tectonic structures, using simple geophysical methods

2011 ◽  
Vol 145 (2-3) ◽  
pp. 159-165 ◽  
Author(s):  
L. Thinova ◽  
A. Fronka ◽  
K. Rovenska
2009 ◽  
Vol 48 (3) ◽  
pp. 311-315 ◽  
Author(s):  
Katalin Nagy ◽  
István Berhés ◽  
Tibor Kovács ◽  
Norbert Kávási ◽  
János Somlai ◽  
...  

Warta Geologi ◽  
2021 ◽  
Vol 47 (3) ◽  
pp. 199-203
Author(s):  
Nik Adib Yaaziz ◽  
◽  
Mohd Hariri Arifin ◽  

Geophysics play a vital role in the constructions of any major manmade structures in the world. One of those being the tunnels. In depth understanding of geophysical methods and a lot of information are needed in order to design a tunnel construction project. Comprehensive investigation on the ground condition has to be done before the field preparation study that will determine the stand-up time and the groundwater condition that may disrupt the tunnel construction. For tunnel stability assessment, an integration of geophysical methods is a must in order to obtain the most accurate results. Satellite imaging interpretation emphasizes on the structural tracing of negative lineament while field mapping emphasizes on location of underground seepage and major tectonic structures such as faults, joints and shear zones. Geoelectrical resistivity tomography survey is able to identify the differences in resistivity of Earth’s materials based on the water content inside of them. The best course of remediation could only be chosen once the output from all these studies are made available.


2012 ◽  
Vol 4 (1) ◽  
Author(s):  
Nadine Hoffmann ◽  
Klaus Reicherter ◽  
Christoph Grützner ◽  
Jochen Hürtgen ◽  
Andreas Rudersdorf ◽  
...  

AbstractLake Ohrid (between FYR of Macedonia and Albania), situated in an active tectonic region of the Balkanides, is characterized by N — S trending active faults. To reconstruct the Holocene shoreline evolution we investigated the coastline using sediment cores and geophysical methods to image sedimentary and tectonic structures. We revealed areas of differing sedimentation regimes. The plains north and south of the lake are dominated by clastic input related to climate variations and uplift/erosion, whereas the steep western and eastern margins are controlled by recent tectonics. Furthermore, no evidence for a much higher lake-level during the Holocene was found in the plains north and south of the lake, except rare temporary floodings. This is supported by mappings of the limestone cliffs around Lake Ohrid, which yielded no evidence for abrasional platforms or notches as indicators for past highstands.


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