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1 day ago · The Aegean region and its graben system constitute one of Turkey’s most significant seismic zones. The faults within the Aegean graben generate numerous earthquakes, leading to various human and economic losses. To better understand the seismicity of western Anatolia, it is necessary to obtain concrete findings regarding the seismic history of earthquake-producing graben faults. This can be ...
5 days ago · Maintenance managers, manufacturing teams and other business leaders in industries where safety, reliability and risk management are critical to operations use fault tree analysis (FTA) to identify and understand the causes of a potential issue before equipment breakdowns occur. This top-down analysis method uses a graphical model to evaluate ...
20 hours ago · Faults are fractures on the Earth’s crust where blocks of rocks move relative to one another. It can be small and localized or hundreds of kilometers long. Active faults are faults that moved within the last 10,000 years and will move again in the future.
4 days ago · Fault management systems are tools to prevent network faults from happening. Their major motto is fault tolerance, and downtime minimization is their main concern. But let’s first understand where those faults come from. Network faults originate from events in the network that have an impact on service delivery.
1 day ago · This study addresses the challenge of maintaining reliability in PV systems by proposing a method to detect and identify simultaneous faults, using kernel principal component analysis (KPCA) and statistical metrics. The proposed method employs KPCA, a machine learning technique adept at identifying patterns in complex data.
5 days ago · Earthquakes are caused by shifts in the outer layers of Earth—a region called the lithosphere. The solid crust and top, stiff layer of the mantle make up a region called the lithosphere. The lithosphere isn’t a continuous piece that wraps around the whole Earth like an eggshell.
20 hours ago · The Philippine fault is a ~1250-km-long, left-lateral strike-slip fault extending NNW parallel to the Philippine archipelago. This fault has been very active in the past 200 years with several destructive earthquakes accompanied by surface rupture.
