![]() Expensive observatory-grade seismic systems are not necessary for seismic hazard deployments or small-scale tomographic studies. ![]() Seismic hazard monitoring in CO2 sequestration fields requires a seismic network over a spatially larger region possibly having stations in remote settings. Another problem that may exist in CO2 sequestration fields is the potential for damaging induced seismicity associated with fluid injection into the geologic reservoir. These types of studies require expensive deployments of surface and borehole sensors in the vicinity of the CO2 injection wells. ![]() Many of these include monitoring underground gas migration through detailed tomographic studies of rock properties, integrity of the cap rock and micro seismicity with time. There are many seismological aspects associated with monitoring of permanent storage of carbon dioxide (CO2) in geologic formations.
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