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Thomas Goebel

Researcher at University of Memphis

Publications -  38
Citations -  1621

Thomas Goebel is an academic researcher from University of Memphis. The author has contributed to research in topics: Induced seismicity & Fault (geology). The author has an hindex of 17, co-authored 35 publications receiving 1040 citations. Previous affiliations of Thomas Goebel include University of Southern California & University of California.

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The 2016 Mw5.1 Fairview, Oklahoma earthquakes: Evidence for long-range poroelastic triggering at >40 km from fluid disposal wells

TL;DR: In this article, the authors examined triggering mechanisms of induced earthquakes, which occurred at more than 40 km from wastewater disposal wells in the greater Fairview region, northwest Oklahoma, employing numerical and semi-analytical poroelastic models.
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Acoustic emissions document stress changes over many seismic cycles in stick-slip experiments

TL;DR: Goebel et al. as mentioned in this paper investigated variations in seismic b value of acoustic emission events during the stress buildup and release on laboratory-created fault zones, and showed that b values mirror periodic stress changes that occur during series of stick-slip events, and are correlated with stress over many seismic cycles.
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Induced earthquake magnitudes are as large as (statistically) expected

TL;DR: In this article, the authors show that the largest earthquakes observed at fluid injection sites are consistent with the sampling statistics of the Gutenberg-Richter distribution for tectonic earthquakes, assuming no upper magnitude bound.
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The spatial footprint of injection wells in a global compilation of induced earthquake sequences

TL;DR: Analysis of spatial seismicity decay in a global dataset of 18 induced cases with clear association between isolated wells and earthquakes finds far-reaching spatial effects during injection may increase event magnitudes and seismic hazard beyond expectations based on purely pressure-driven seismicity.
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Identifying fault heterogeneity through mapping spatial anomalies in acoustic emission statistics

TL;DR: In this article, the authors studied stick-slip sequences in an analog, laboratory setting to investigate how microseismicity is linked to fault heterogeneities and the occurrence of dynamic slip events, and found that geometric asperities identified in CT scan images were connected to regions of low b values, increased event densities and moment release over multiple stick slip cycles.