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At the time, earthquakes were a relatively rare event for Oklahomans.
A little online research revealed that 2001 was the last time earthquakes hit the city.
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We investigate the time synchronization of faults analyzing the statistical distribution of interevent times, i.e.,, where is the time occurrence of the ith earthquake on the OP-fault, is the time occurrence of the closest in time earthquake on the F-fault, and.
In this case, we may either observe a marked time synchronization between faults or a significant probability gain; i.e., the occurrence of an earthquake on F-fault increases significantly the probability to have a close in time earthquake on OP-fault.
In ancient times earthquakes, famines or floods were seen as inevitable signs that the mandate had been withdrawn.
Multiple news broadcasts are playing simultaneously, and a real-time earthquake map is tracking the region's seismic activity.
This paper has studied the key issues about integration of GNSS and strong-motion records for real-time earthquake monitoring.
A web portal was developed to integrate the real-time geospatial web services reporting with real-time earthquake related information for spatial policy analysis and collaborative decision-making.
These ideas give an important guide for real-time earthquake monitoring and early warning by the tight integration of GNSS and strong-motion records.
In this exploratory effort, the USGS is developing a system that gathers real-time, earthquake-related messages from the social networking site Twitter and applies place, time, and key word filtering to gather geo-located accounts of shaking.
Statistical models for describing the occurrence process of earthquakes can be used for short-term or real-time earthquake forecasts (Vere-Jones, 1970).
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