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This suggests that the high-temperature area around the magma chamber might have contributed to the termination of the rupture of the mainshock.
The high-temperature area around the magma chamber of Mt. Aso may have contributed to the termination of the rupture during the mainshock and the low aftershock activity around the Aso volcano.
Plot for Peace carefully and beautifully places together all the pieces of the puzzle that contributed to the termination of the apartheid regime in South Africa and the release of indisputable world hero Nelson Mandela.
Unconfirmed Soviet bomber threats, the overwhelming trend toward offensive and defensive nuclear missiles in the late 1950s and early 1960s, as well as rising costs, contributed to the termination of the XF-108.
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He said Aetna would consider any actions which were consistent with its previously announced strategic review and that "might contribute to the termination of litigation".
Hence, the two direct CRC targets, YUC4 and TRN2, cooperatively contribute to the termination of floral meristem development through WUS regulation (Fig. 7k).
We also showed that two auxin-related direct CRC targets, YUC4 and TORNADO2, cooperatively contribute to the termination of floral stem cell maintenance.
Furthermore, the viscous rheology of the mixture of gas, melt, and crystals, which causes the low density of the SLDB, also contributes to the termination of the rupture: A viscous rheology inhibits rupture beneath the caldera.
The high-temperature area around the magma chamber of Mt. Aso may contribute to the termination of the rupture during the mainshock and peculiarly low aftershock activity of the 2016 Kumamoto earthquake, around Mt. Aso.
Using the 2011 eruption of Shinmoe-dake as an example, and by examining the dependency of the magma discharge rate on the chamber pressure, we consider how a change in the chamber pressure contributes to the termination of the effusive eruption.
Yagi et al. (2016) estimated the source rupture process of the mainshock using teleseismic records and showed that the northeast edge of the large-slip area is located in this region, suggesting that the high-temperature area around the magma chamber of Mt. Aso contributes to the termination of the rupture during the mainshock.
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