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Abstract

During fluid-injection tests in boreholes a spontaneons seismic emission (microearthquakes) can be induced in rocks. We assume that these seismic microevents are due to the perturbation of the porous pressure caused by the fluid injection.

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/content/papers/10.3997/2214-4609.201408158
1998-06-08
2023-09-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408158
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