Publications by authors named "S V Filatov"

Article Synopsis
  • Territories in southern Eastern Europe and the Caucasus are affected by tick-borne relapsing fever (TBRF), which is caused by the Borrelia caucasica spirochete transmitted by Ornithodoros verrucosus ticks.
  • A study involving the mitochondrial genomes of 54 O. verrucosus ticks from 23 populations in Ukraine, Georgia, and Azerbaijan revealed 47 unique haplotypes, indicating distinct genetic diversity and minimal gene flow among populations.
  • The research identified four evolutionary lineages of the ticks, showing that environmental factors, along with geographic distance, may contribute to the divergence of these tick populations over time.
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We extend Bloch sphere formalism to pure two-qubit systems. Combining insights from Geometric Algebra and the analysis of entanglement in different conjugate bases we identify two Bloch sphere geometry that is suitable for representing maximally entangled states. It turns out that the relative direction of the coordinate axes of the two Bloch spheres may be used to describe the states.

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Previous research has implicated ticks, including , as long-term reservoirs of relapsing fever (RF) spirochetes. Considering the tick's long lifespan and their efficiency in maintaining and transferring spirochetes within the population, the infection could persist in a given enzootic focus for decades. However, little is known about the relative importance of horizontal and vertical transmission routes in the persistence and evolution of RF .

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The accuracy of the ion flight time measurement in the time-of-flight mass spectrometer is critical to achieving high resolution. The pulse amplitude variation of the detector pulses leads to the registration time spread at a given pulse detection threshold. This time spread can be eliminated by determining the position of the pulse apex.

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This paper reports an investigation of the chemistry, crystal structure refinement and thermal behavior (80-1650 K) of ludwigite from the Iten'yurginskoe deposit (Eastern Chukotka, Russia). Its chemical composition was determined by electron microprobe analysis, giving an empirical formula (MgFeMn)(FeAlMg)O(BO). A refinement of the crystal structure from single-crystal X-ray diffraction data (SCXRD) was provided for the first time for ludwigite from this deposit (R = 0.

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