The recent seismicity at the Alp-Dinarides Junction

From Figure 4(a) and 4(b), it is possible to notice that at both levels of layer thickness, a minimum quantity of energy density should be delivered to the powder in order to obtain

Figure 1(b) shows the double-Gaussian model fit to the differential asymmetry for the simulated samples.. 1(a) shows that the double-Gaussian model matches all the simulated

Marco, S., 2007, Temporal variation in the geometry of a strike-slip fault zone: Examples from the Dead Sea Transform: Tectonophysics, v. Marco, S., Rockwell, T.K., Heimann,

The implementation of the Life Project required that a monitoring of the habitat quality was carried out, to verify the efficaciousness of the actions

The analysis of seismic activity distribution in the years 2007-2016 for individual GZW structural units indicates that the tremors are generated by mining operations

The Technical-Scientific Commission for evaluating the possible relationships between hydrocarbon exploration and a marked increase of seismicity in the Emilia Romagna area

To locate seismic events, we used the algorithm NLLoc (Non Linear Location, Lomax et al., 2009), while tomographic inversion has been performed using the Cat3D software (Computer

compute the total cost function, the average cost function and the marginal cost