scholarly journals Characterizing the Normative Voice Tremor Frequency in Essential Vocal Tremor

2018 ◽  
Vol 144 (12) ◽  
pp. 1169 ◽  
Author(s):  
Cristen Paige ◽  
Bridget L. Hopewell ◽  
Vahram Gamsarian ◽  
Brett Myers ◽  
Priyesh Patel ◽  
...  
1999 ◽  
Vol 72 (2-4) ◽  
pp. 241-244 ◽  
Author(s):  
Michael S. Yoon ◽  
Michael Munz ◽  
Robert T. Sataloff ◽  
Joseph R. Spiegel ◽  
Reinhardt J. Heuer

2007 ◽  
Vol 97 (5) ◽  
pp. 3219-3228 ◽  
Author(s):  
Jan Raethjen ◽  
R. B. Govindan ◽  
Florian Kopper ◽  
M. Muthuraman ◽  
Günther Deuschl

Conflicting results on the existence of tremor-related cortical activity in essential tremor (ET) have raised questions on the role of the cortex in tremor generation. Here we attempt to address these issues. We recorded 64 channel surface EEGs and EMGs from forearm muscles in 15 patients with definite ET. EEG and EMG power spectra, relative power of the rhythmic EMG activity, relative EEG power at the tremor frequency, and EEG–EMG and EEG–EEG coherence were calculated and their dynamics over time explored. Corticomuscular delay was studied using a new method for narrow-band coherent signals. Corticomuscular coherence in the contralateral central region at the tremor frequency was present in all patients in recordings with a relative tremor EMG power exceeding a certain level. However, the coherence was lost intermittently even with tremors far above this level. Physiological 15- to 30-Hz coherence was found consistently in 11 patients with significantly weaker EMG activity in this frequency range. A more frontal (mesial) hot spot was also intermittently coupled with the tremor and the central hot spot in five patients. Corticomuscular delays were compatible with transmission in fast corticospinal pathways and feedback of the tremor signal. Thus the tremor rhythm is intermittently relayed only in different cortical motor areas. We hypothesize that tremor oscillations build up in different subcortical and subcortico-cortical circuits only temporarily entraining each other.


2011 ◽  
Vol 198 (1) ◽  
pp. 110-113 ◽  
Author(s):  
Zdenka Uhríková ◽  
Otakar Šprdlík ◽  
Martina Hoskovcová ◽  
Arnošt Komárek ◽  
Olga Ulmanová ◽  
...  

1987 ◽  
Vol 1 (2) ◽  
pp. 162-167 ◽  
Author(s):  
Lorraine A. Ramig ◽  
Thomas Shipp
Keyword(s):  

2016 ◽  
Vol 142 (2) ◽  
pp. 117 ◽  
Author(s):  
Andrew Nida ◽  
Josie Alston ◽  
John Schweinfurth
Keyword(s):  

1972 ◽  
Vol 62 (2) ◽  
pp. 481-492 ◽  
Author(s):  
Harsh K. Gupta ◽  
B. K. Rastogi ◽  
Hari Narain

abstract A detailed examination of the behavior of earthquakes associated with over a dozen artificial lakes shows that, in all cases, the tremors were initiated or their frequency increased considerably following the lake filling and that their epicenters were mostly located within a distance of 25 km from the lakes. Among the factors affecting the tremor frequency are the rate of increase of water level, duration of loading, maximum levels reached, and the period for which the high levels are retained. The study of these reservoir-associated earthquake sequences reveals that the ratio of the largest aftershock to the main shock is high (about 0.9), and the b values are also high in the frequency-magnitude relation, which is contrary to the normal earthquakes of the concerned regions.


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