Gif Recorder 3.2.1.0 Patch: Tips and Tricks for Making Awesome GIFs

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Gif Recorder 3.2.1.0 Patch

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The fact that the 2012 earthquake occurred essentially in the middle of our observation networks provides an incredible research opportunity. Data from the continuous GPS network is archived at UNAVCO and is publicly available. I encourage anyone with an interest in seismic processes and high precision geodetic data to use these data in their research (UNAVCO). Rapid time series analysis results from the ARIA project at the Jet Propulsion Lab. 5 Hz GPS data are also available for selected stations (see UNAVCO web site). These high rate position/displacement data can give important information on the high amplitude crustal displacements that happen in the immediate aftermath of an earthquake, a time when conventional seismometers can saturate (go off scale). This information is critical for understanding the stresses on buildings and other infrastructure during earthquakes. Special instruments (called strong motion recorders) are the preferred way to measure these signals, but may not always be available. High precision time series (based on high precision satellite ephemeris data) and other results will be posted to this website as they become available.

In addition to process-oriented research, there are more immediate hazard-related aspects for this event to be considered. The apparent rupture area of the earthquake is smaller than the locked patch we infer from recent GPS-based models, and rather deep ( 40 km). This raises the possibility of a second earthquake in the near future, rupturing up-dip of the current event. Being shallower than the September 5 event, the subsequent event could be more damaging, and perhaps stimulate a tsunami (there was no significant tsunami associated with the September 5 event). The role of past and future slow slip events at relieving some of this accumulated strain is only poorly known.

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