Peter Geiser, Alfred Lacazette and Jan Vermilye introduce tomographic fracture imaging (TFI) as a new semblance-based tool using surface seismic networks to directly map both the natural and induced fracture systems of the Earth’s brittle crust. In contrast to microseismic data consisting solely of hypo-centres TFI is said to have the ability to obtain images of the actual fractures themselves.
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Geiser et al. (2012) studied this question.
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