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Transcript
Felix Waldhauser, Lamont-Doherty Earth Observatory
Title:
Deciphering the Fabric of Seismicity: Implications for Earthquake and Plate Tectonic
Processes.
Abstract:
Seismic monitoring systems detect and locate tens of thousands of earthquakes
every year, adding to an ever growing archive of instrumentally recorded seismic
data that goes back almost a century. Most of the world’s earthquakes occur along
the boundaries of tectonic plates and represent the primary physical expression of
plate tectonic processes. The location of earthquakes within the Earth’s crust and
mantle are the fundamental parameters used in a wide range of research areas,
including earthquake physics, the structure and dynamics of the Earth’s interior, and
seismic hazards. Yet, the accuracy with which we know these locations is typically
poor, and often unknown. Using advanced analysis techniques that harness both the
vast amount of digital seismic data and increasing computing power, we can image
seismicity at a much higher resolution and across larger regions than has previously
been possible. In this talk I will describe recent developments in high-precision
earthquake location techniques and their use towards real-time monitoring of
seismogenic properties. I will present results from using these methods at both local
to global scales to study the three-dimensional structure of active fault systems, the
spatio-temporal evolution of seismicity, and the physical processes underlying
seismic failure along major plate boundaries.