Encyclopedia of Exploration Geophysics 2014

DOI: 10.1190/1.9781560803027.entry5

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5. Seismic Interferometry

Gerard T. Schuster¹

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Cited by 7 publications

References 182 publications

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Geophysical Subsoil Characterization of a Housing Unit Shaken by the Earthquake of September 19, 2017 (Mw 7.1)

Cárdenas‐Soto¹,

Sánchez-Gónzalez²,

Martínez-González³

et al. 2020

Preprint

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Geophysical Subsoil Characterization of a Housing Unit Shaken by the Earthquake of September 19, 2017 (Mw 7.1)

Cárdenas‐Soto¹,

Sánchez-Gónzalez²,

Martínez-González³

et al. 2020

Preprint

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No abstract

Ambient Noise Surface Wave Reverse Time Migration for Fault Imaging

¹

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²

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³

et al. 2020

JGR Solid Earth

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Faults are basic components of subsurface structures that represent discontinuities in physical properties. In addition to being the controlling factor of major tectonic earthquakes (e.g., Angelier, 1990; Martin et al., 2016; Sibson, 1983), subsurface faults also play an essential role in natural resources, including hydrocarbon accumulation and formation of oil and gas reservoirs (Aydin, 2000), aggregation of metallic ore deposits (e.g., Goldfarb et al., 2005; Spencer & Welty, 1986), and generation of geothermal reservoirs (Chen & Huang, 2015). Therefore, detailed characterization of subsurface faults is crucial for understanding tectonic activities and for exploring natural resources. Many geophysical approaches for fault delineation have been proposed in the past decades, such as gravity, magnetic, electromagnetic, and seismic methods (e.g.,

Subsurface seismic imaging using drill bit noise

¹

,

³

et al. 2019

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