This paper presents a novel fault location method for series compensated transmission lines. It is established based on synchronized voltages sampling and Thevenin impedance from both ends of series compensated transmission line. The method is based on the use of phasor measurement units (PMU) technology which is aimed to be independent of current measurements, fault type, fault resistance, fau...

A detailed 3-D P-wave velocity structure of the crust in the epicentral area of the 17 January, 1994 Northridge earthquake is determined by using 104,709 arrival times from 1673 Northridge aftershocks and 2948 other local earthquakes. A test performed using the data from the nearby portable stations suggests that the aftershock hypocenters relocated with the obtained 3-D model are accurate to a...

In this research seismicity parameters, repeat times and occurrence probability of large earthquakes are estimated for 35 seismic lineaments in Persian plateau and the surrounding area. 628 earthquakes of historical time and present century with MW>5.5 were used for further data analysis. A probabilistic model is used for forecasting future large earthquake occurrences in each chosen lineament....

We describe the morphology of a large and complex graben structure in the western Thauma-sia region (the " Thaumasia graben " [1] or TG). We consider possible fault geometries, determine extension , and discuss shortly possible models for its origin. Background: Situated at the western border of the Thaumasia plateau, the TG is one of the most prominent fault-bounded structures on Mars. It is ~...

Highly available and resilient networks play a decisive role in today’s networked world. As network faults are inevitable and networks are becoming constantly intricate, finding effective fault recovery solutions in a timely manner is becoming a challenging task for administrators. Therefore, an automated mechanism to support fault resolution is essential towards efficient fault handling proces...

Geological structures in the Bukit Gadang geothermal area have been identified using geomagnetic method to determine type of fault. Data was measured a magnetometer with dimensions 1200 m × consisting 144 points at 12 tracks, and spacing between 100 m. Magnetic anomaly data performed diurnal IGRF (International Geomagnetic Reference Field) corrections. Furthermore, reduced poles continuous upwa...

The 17 of August 1999, an important earthquake of magnitude 7.6 occurred along the North Anatolian fault in the area of Izmit (Turkey). Relative horizontal displacements up to 4.5 meters were observed. The epicenter of the earthquake under concern is located in Golcuk, near the city of Izmit, on the South border of the Marmara Sea. The fault in the vicinity of Izmit is mainly oriented along an ...