BADANIA GEOFIZYCZNE I MODELOWANIE DLA ROZPOZNANIA KRASU GIPSOWEGO-1 -2 3 -Brought to you by | University of Manitoba Authenticated Download Date | 6/8/15 2:29 PM
The paper presents the results of geophysical research conducted in the region where the so called ‘Gold Train’ was believed to be located. The surveyed site was located in Wałbrzych, at the 65th kilometre of the railway connecting Wrocław and Wałbrzych. The aim of the research was to verify the legend of the existence of the so called ‘Gold Train’ that was supposed to be located in the tunnel. The ‘Gold Train’ was believed to contain Wrocław's treasures. Three geophysical methods were used. Microgravimetric and GPR (ground‐penetrating radar) methods were applied to locate the void (tunnel), while the search for the train (a metal object) was conducted with the use of a magnetic method. Detailed geodetic measurements were used, including, among others, laser scanning. Due to complex terrain and geological structure, the negative results of the microgravimetric research was conclusive only in respect of one of the profiles. Due to high attenuation of electromagnetic wave by a shallow geological structure the scope of the GPR method was limited, however it was sufficient to confirm that such a tunnel does not exist. Despite difficulties related to electric lines in the researched area, conclusive results were obtained using the magnetic method. No magnetic anomaly with a shape or amplitude indicative of a steel train was identified.
The Pieniny Klippen Belt (PKB) is located in the suture zone between the Central and Outer (Flysch) Carpathians. Its structure is an effect of prolonged processes of the Cretaceous–Miocene folding, thrusting and uplifting. In this zone, tectonic components of different ages and features, including strike-slip-bounded tectonic blocks, thrust units, as well as toe-thrusts and olistostromes, result in the present-day mélange characteristics of the PKB, where individual tectonic units are difficult to distinguish. In the PKB, both tectonic and sedimentary events triggered the mélange creation. The name “Klippen Belt” is derived from cliffs (German Klippen). These cliffs form harder, more erosion-resistant elements of the mélange, residing within less competent clastic deposits, sandstones, shales and marls that form flysch complexes. The cliffs often represent olistoliths, which glided down from elevated areas to the deeper basinal zones. Two olistostrome belts were distinguished. The older one resulted from subduction of the southern part of the Alpine Tethys, and the younger originated in response to the northward shift of the accretionary wedge. The other cliffs were placed within the surrounding clastic by tectonic deformational processes. The flower structure of the PKB was formed during the collision and strike-slip movement of the lithospheric plates. This structure is limited on both sides by deep-rooted faults. Several evolutionary stages could be distinguished in these areas. The rift-related stage is expressed by the opening of the Alpine Tethys that contains two major basins—Magura and Pieniny (Złatne) basins, separated by Czorsztyn Ridge. The reorganization of the Alpine Tethys basins and the development of the accretionary prism happened during the synorogenic stage. This process was initiated by the movement of the Central Carpathians. Thick flysch sequences with olistostromes were deposited in these basins. The Czorsztyn Ridge was destroyed during the late orogenic stages.
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