Add to ORKGOn the basis of stress accumulation between two large earthquakes the maximum strain rate can be estimated. But the strain rates cannot be used to estimate directly the magnitude of the tectonic processes. The estimates of stress rates and horizontal crustal movement values are bigger than the real values in nature. Due to the significant differences among stations situated in the same region it seems that secular rates are modified or increased to a considerable extent by local conditions of different type, which are not connected to tectonic activity. ARK: https://n2t.net/ark:/88439/y092577 Permalink: https://geophysicsjournal.com/article/15  
Two critical items in the energetic budget of a seismic province are the strain rate, which is measu...
The state and the magnitude of stress in the Earth's lithosphere have an important bearing on vario...
The state and the magnitude of stress in the Earth's lithosphere have an important bearing on vario...
A value of ∼10−14 s−1 is commonly cited as an average geological strain rate. This value was fir...
The strain-rebound characteristic of the sequence of all great shallow earthquakes of magnitudes 8.0...
Earthquakes are caused by the release of tectonic strain accumulated between events. Recent advances...
In this article, we first review the progress in our understanding of tectonic stresses in the Earth...
The abrupt changes of the crustal strains during the earthquakes have been observed with some compon...
Long-period horizontal seismometers, tiltmeters and strainmeters are influenced by inhomogeneous roc...
Abstract. Although the average strain rates within stable continental regions (SCR) are 2-3 orders o...
cited By 2Stresses in the Earth's crust are known to represent a key element of geodynamical process...
cited By 2Stresses in the Earth's crust are known to represent a key element of geodynamical process...
A value of ∼10−14 s−1 is commonly cited as an average geological strain rate. This value was fir...
Earthquakes are caused by the release of tectonic strain accumulated between events. Recent advances...
A value of ∼10−14 s−1 is commonly cited as an average geological strain rate. This value was fir...
Two critical items in the energetic budget of a seismic province are the strain rate, which is measu...
The state and the magnitude of stress in the Earth's lithosphere have an important bearing on vario...
The state and the magnitude of stress in the Earth's lithosphere have an important bearing on vario...
A value of ∼10−14 s−1 is commonly cited as an average geological strain rate. This value was fir...
The strain-rebound characteristic of the sequence of all great shallow earthquakes of magnitudes 8.0...
Earthquakes are caused by the release of tectonic strain accumulated between events. Recent advances...
In this article, we first review the progress in our understanding of tectonic stresses in the Earth...
The abrupt changes of the crustal strains during the earthquakes have been observed with some compon...
Long-period horizontal seismometers, tiltmeters and strainmeters are influenced by inhomogeneous roc...
Abstract. Although the average strain rates within stable continental regions (SCR) are 2-3 orders o...
cited By 2Stresses in the Earth's crust are known to represent a key element of geodynamical process...
cited By 2Stresses in the Earth's crust are known to represent a key element of geodynamical process...
A value of ∼10−14 s−1 is commonly cited as an average geological strain rate. This value was fir...
Earthquakes are caused by the release of tectonic strain accumulated between events. Recent advances...
A value of ∼10−14 s−1 is commonly cited as an average geological strain rate. This value was fir...
Two critical items in the energetic budget of a seismic province are the strain rate, which is measu...
The state and the magnitude of stress in the Earth's lithosphere have an important bearing on vario...
The state and the magnitude of stress in the Earth's lithosphere have an important bearing on vario...