Diatom succession in the post-glacial sediments of the Komořany Lake, North-West Bohemia, Czechoslovakia

Hydrobiologia ◽  
1983 ◽  
Vol 103 (1) ◽  
pp. 241-245 ◽  
Author(s):  
Zdeňka Řeháková
2018 ◽  
Author(s):  
Marius Kriegerowski ◽  
Simone Cesca ◽  
Matthias Ohrnberger ◽  
Torsten Dahm ◽  
Frank Krüger

Abstract. We develop an amplitude spectral ratio method for event couples from clustered earthquakes to estimate seismic wave attenuation (Q−1) in the source volume. The method allows to study attenuation within the source region of earthquake swarms or aftershocks at depth, independent of wave path and attenuation between source region and surface station. We exploit the high frequency slope of phase spectra using multitaper spectral estimates. The method is tested using simulated full wavefield seismograms affected by recorded noise and finite source rupture. The synthetic tests verify the approach and show that solutions are independent of focal mechanisms, but also show that seismic noise may broaden the scatter of results. We apply the event couple spectral ratio method to North-West Bohemia, Czech Republic, a region characterized by the persistent occurrence of earthquake swarms in a confined source region at mid-crustal depth. Our method indicates a strong anomaly of high attenuation in the source region of the swarm with an averaged attenuation factor of Qp 


2014 ◽  
Vol 17 (4) ◽  
pp. 579-601 ◽  
Author(s):  
Jaroslav Řídký ◽  
Markéta Končelová ◽  
Radka Šumberová ◽  
Petr Limburský ◽  
Petr Květina

The aim of this study is to analyse the correlation between finds and ditches, the duration of ditch fills, and the manner of the demise of Late Neolithic rondels (Kreisgrabenanlagen) in the Czech Republic. Two comparable long-term projects are discussed here: Kolín (central Bohemia) and Vchynice (north-west Bohemia). Qualitative, quantitative, and spatial analyses of the different categories of finds (pottery fragments, lithics, daub, and faunal remains) from the ditch fills show that only finds from the bottom layers of the ditches were contemporary with the primary function of the rondels. However, the bottom layers often only contained a few artefacts. The richest parts of the ditches, the middle and upper layers, from both sites illustrated similar characteristics: after the rondels lost their primary function, the ditches were filled by both natural and cultural agents over a long period. As a consequence, some previous, and widely accepted, interpretations of the relationship between individual areas of rondels and their relationship with surrounding features, as well as the relationship of the finds from ditch fills to rondel function and chronology, need to be revisited.


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