Abstract
The Ebersbrunn diatreme is a deeply eroded (>1 km) diatreme structure in western Saxony, Germany. At current erosion levels, this ultramafic to carbonatitic diatreme is about 2 × 1.5 km in map view, which makes it a large one. Based on shallow drill cores, the diatreme contains coarse unbedded volcaniclastic rocks with up to 80 % country rock fragments. The diatreme is characterised by positive and negative magnetic anomalies, which are controlled mostly by the changing proportions of magnetic minerals in the rocks. The magnetic minerals are themselves contained in the juvenile fraction. Rock magnetic studies on three drill cores, one from the magnetic low and two from magnetic highs, including bulk susceptibility and its anisotropy, temperature dependent susceptibility, various remanence measurements (natural remanent magnetisation, anhysteretic remanence and isothermal remanent magnetisation) and alternating field demagnetisation have been performed. Additionally scanning electron microscope imaging and energy-dispersive X-ray spectroscopy were performed to better characterise the magnetic minerals. Magnetisation is caused by titanomagnetite with slightly varying Ti contents within all cores. Samples from the positive magnetic anomalies have a relatively high degree of anisotropy, but no preferred orientation of one of the principal axes can be seen. The magnetic highs are caused by non-bedded volcaniclastic rocks comparatively rich in juvenile particles. The negative magnetic anomaly is associated with a compaction-like magnetic fabric but without macroscopically visible bedding. Hence, the magnetic low is caused by rocks with a lower content of juvenile material. To the authors’ knowledge, this is the first time rock magnetic methods have been applied to diatreme rocks.
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Acknowledgements
First of all, the authors would like to dedicate this paper to W. Jäger and K. Hoth who preserved the drill cores during the political change in the late 1980s and early 1990s in East Germany. We would like to thank D. Markwart and H. Matthes who aquired geomagnetic and gravimetric field data. We would also like to express our gratitude to C. Kroner (Physikalisch-Technische Bundesanstalt Braunschweig) for the initial surveys prior to our measurements. All the staff of GFZ Potsdam who helped in this project, especially H. Liep, S. Gehrmann and T. Nickschick, are kindly thanked for their work. Sincere thanks to P. Suhr, M. Lapp, P. Wolf and H. J. Berger from the Sächsisches Landesamt für Umwelt, Landwirtschaft und Geologie for the access and the possibility to sample the drill cores as well as for the critical and stimulating discussions. A. Hiller (geological archive of the Wismut GmbH, Chemnitz) is thanked for literature research. This study was founded by the German Research Foundation (DFG), Project KA 902/17-1, JA 542/21-1 and the Deutsches GeoForschungsZentrum GFZ. We thank journal reviewers Helga de Wall and Conall Mac Niocaill for helpful comments. We also thank very much the handling editor Pierre-Simon Ross for his critical comments that helped us to improve the manuscript.
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Smith IEM, Nemeth K, and Ross P-S (eds) Monogenetic volcanism and its relevance to the evolution of volcanic fields.
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Schmidt, A., Nowaczyk, N., Kämpf, H. et al. Origin of magnetic anomalies in the large Ebersbrunn diatreme, W Saxony, Germany. Bull Volcanol 75, 766 (2013). https://doi.org/10.1007/s00445-013-0766-6
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DOI: https://doi.org/10.1007/s00445-013-0766-6