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Since the comprehensive borehole crustal activity observation device is also equipped with seismometers, the waveforms observed by the seismometers are also shown for reference.
This paper presents the analysis of 14 years of cloud-to-ground lightning activity observation in Colombia using lightning location systems (LLS) data.
Therefore, the comprehensive crustal activity observation device incorporating the stress meter and other components is fixed inside a deep borehole with expansible grout.
The stress meter is usually used as a component incorporated in the comprehensive crustal activity observation device that we have developed.
We have developed a comprehensive borehole crustal activity observation device (comprehensive observation device) equipped with strain meters and also tiltmeters, seismometers, and other components that are all co-located in one borehole container.
Figure 12 shows the stress seismic motion waveforms recorded by the stress meter in the comprehensive crustal activity observation device at the TOS borehole station (depth of 512 m) during the 2011 Tohoku earthquake (M 9.0), which occurred on 11 March 2011.
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During activity observations, movement was generally observed as a single short distance jet followed by a brief rest, then another short jet in a seemingly random direction.
The downward adjustment of the flare frequency based on the activity measurements leads to a better agreement between astrophysical activity observations of superflare stars and the frequency of solar flares recorded in geological archives (see Fig. 7 for details).
Docking studies reveal the possibility of both hetero- (S-Cit + 5-HT) and homo-dimeric (5-HT + 5-HT) co-binding at both these sites which may explain earlier published allosteric activity observations and provide novel design strategies.
We present some preliminary studies, in which, through theoretical dynamo modeling and analysis of magnetic activity observations of solar-like stars at various evolutionary phases relative to the Sun, we show how the above concept is implemented in practice.
In this study, we describe seafloor seismic monitoring of Nishinoshima volcano using LT-OBSs and present Nishinoshima volcanic activity observations from February 2015 to May 2017.
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