Please use this identifier to cite or link to this item: http://dx.doi.org/10.14279/depositonce-8114
Main Title: High-resolution shear-wave seismic reflection as a tool to image near-surface subrosion structures – a case study in Bad Frankenhausen, Germany
Author(s): Wadas, Sonja Halina
Polom, Ulrich
Krawcyk, Charlotte M.
Type: Article
Language Code: en
Is Part Of: 10.14279/depositonce-7247
Abstract: Abstract. Subrosion is the subsurface leaching of soluble rocks that results in the formation of depression and collapse structures. This global phenomenon is a geohazard in urban areas. To study near-surface subrosion structures, four shear-wave seismic reflection profiles, with a total length of ca. 332m, were carried out around the famous leaning church tower of Bad Frankenhausen in northern Thuringia, Germany, which shows an inclination of 4.93° from the vertical. Most of the geological underground of Thuringia is characterized by soluble Permian deposits, and the Kyffhäuser Southern Margin Fault is assumed to be a main pathway for water to leach the evaporite. The seismic profiles were acquired with the horizontal micro-vibrator ELVIS, developed at Leibniz Institute for Applied Geophysics (LIAG), and a 72m long landstreamer equipped with 72 horizontal geophones. The high-resolution seismic sections show subrosion-induced structures to a depth of ca. 100m and reveal five features associated with the leaching of Permian deposits: (1) lateral and vertical varying reflection patterns caused by strongly heterogeneous strata, (2) discontinuous reflectors, small offsets, and faults, which show the underground is heavily fractured, (3) formation of depression structures in the near-surface, (4) diffractions in the unmigrated seismic sections that indicate increased scattering of the seismic waves, and (5) varying seismic velocities and low-velocity zones that are presumably caused by fractures and upward-migrating cavities. A previously undiscovered southward-dipping listric normal fault was also found, to the north of the church. It probably serves as a pathway for water to leach the Permian formations below the church and causes the tilting of the church tower. This case study shows the potential of horizontal shear-wave seismic reflection to image near-surface subrosion structures in an urban environment with a horizontal resolution of less than 1m in the uppermost 10–15m.
URI: https://depositonce.tu-berlin.de//handle/11303/8994
http://dx.doi.org/10.14279/depositonce-8114
Issue Date: 2016
Date Available: 16-Jan-2019
DDC Class: 550 Geowissenschaften
Subject(s): seismic reflection
subrosion
License: https://creativecommons.org/licenses/by/3.0/de/
Journal Title: Solid Earth
Publisher: Copernicus
Publisher Place: Göttingen
Volume: 7
Publisher DOI: 10.5194/se-7-1491-2016
Page Start: 1491
Page End: 1508
EISSN: 1869-9529
ISSN: 1869-9510
Appears in Collections:Inst. Angewandte Geowissenschaften » Publications

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