Abstract:In the Sichuan Basin, seismic activity has been low historically, but in the past few decades, a series of moderate to strong earthquakes have occurred. Especially since 2015, earthquake activity has seen an unprecedented continuous growth trend, and the magnitude of events is increasing. Following the M5.7 Xingwen earthquake on 18 Dec. 2018, which was suggested to be induced by shale gas hydraulic fracturing, a swarm of earthquakes with a maximum magnitude up to M6.0 struck Changning and the surrounding count… Show more
“…All earthquakes are within 2 km to injection wells, which suggest that the earthquakes are very likely to be induced by injection activities. Similar to the 2018 Xingwen earthquake, W1 and W3 are probably nucleated within a zone of elevated pore pressure near injection wells and rupture unidirectionally to the northeast beyond the zone (Lei et al, 2020).…”
On 7 September 2019, an M L 5.4 earthquake struck the Weiyuan area in southwestern China. This is the largest and most damaging event in the Weiyuan shale gas field. In the next 4 months, two earthquakes with M L 4.3 and M L 5.2 rattled the same area. In this study, we obtain source parameters of these earthquakes (e.g., centroid location, focal mechanism, and rupture directivity) to investigate whether they are induced by hydraulic fracturing of shale gas production. We first invert for high-resolution centroid locations and focal mechanisms of two M~3 earthquakes recorded by a temporary dense seismic array. We then adopt the M~3 events as references to obtain reliable centroid locations and rupture directivity of those moderate-size earthquakes. The results show that all earthquakes have centroid depths of no more than 3 km and are within 2 km to injection wells of shale gas production, which suggest that these earthquakes may be induced by local hydraulic fracturing. The M L 5.2 earthquake has the same rupture directivity to NE as the M L 5.4 event and is located in the zone of positive Coulomb stress change caused by the latter. However, the long time lapse of the M L 5.2 earthquake and the existence of an injection well within 2 km suggest that it is more likely induced by hydraulic fracturing than triggered statically by the M L 5.4 earthquake.
“…All earthquakes are within 2 km to injection wells, which suggest that the earthquakes are very likely to be induced by injection activities. Similar to the 2018 Xingwen earthquake, W1 and W3 are probably nucleated within a zone of elevated pore pressure near injection wells and rupture unidirectionally to the northeast beyond the zone (Lei et al, 2020).…”
On 7 September 2019, an M L 5.4 earthquake struck the Weiyuan area in southwestern China. This is the largest and most damaging event in the Weiyuan shale gas field. In the next 4 months, two earthquakes with M L 4.3 and M L 5.2 rattled the same area. In this study, we obtain source parameters of these earthquakes (e.g., centroid location, focal mechanism, and rupture directivity) to investigate whether they are induced by hydraulic fracturing of shale gas production. We first invert for high-resolution centroid locations and focal mechanisms of two M~3 earthquakes recorded by a temporary dense seismic array. We then adopt the M~3 events as references to obtain reliable centroid locations and rupture directivity of those moderate-size earthquakes. The results show that all earthquakes have centroid depths of no more than 3 km and are within 2 km to injection wells of shale gas production, which suggest that these earthquakes may be induced by local hydraulic fracturing. The M L 5.2 earthquake has the same rupture directivity to NE as the M L 5.4 event and is located in the zone of positive Coulomb stress change caused by the latter. However, the long time lapse of the M L 5.2 earthquake and the existence of an injection well within 2 km suggest that it is more likely induced by hydraulic fracturing than triggered statically by the M L 5.4 earthquake.
“…A better understanding of the spatial distribution of hydraulic parameters can facilitate more manageable and optimized operations for these utilizations (Miller et al., 2017). Moreover, the parameters are essential for understanding the scale of hydromechanical responses and its role in fluid injection induced seismicity (Guglielmi et al., 2020; Jiang et al., 2020; Keranen et al., 2014; Lei et al., 2020; Shirzaei et al., 2016; Verdon et al., 2015). Hydrogeologists have long pursued an understanding of the spatial structure of hydraulic parameters in aquifer formation.…”
• Small poroelastic deformation during aquifer testing was monitored using a high-resolution distributed strain sensing (DSS) tool • DSS data are used to inversely estimate the vertical profiles of permeability and compressibility through a coupled hydromechanical model • DSS and inverse modeling are useful for subsurface reservoir characterization and management
“…The Sichuan Basin provided typical cases, in which both long‐term and short‐term injections have caused noticeable (“felt”) induced seismicity, including some destructive earthquakes. Some large earthquakes, such as the M 5.7 (in this article M indicates M L for events of M L < 5 and M S for events of Ms ≥ 5) earthquake on 18 December 2018 induced by shale gas hydraulic fracturing (HF) (Lei et al, 2019a), the M 6.0 earthquake on 17 July 2019 (possibly induced by long‐term injection for salt production) (Lei et al, 2019b), and several earthquakes of M 4.3 to M 5.4 induced by shale gas HF at the Weiyuan‐Rongxian shale gas site (Lei et al, 2020), caused more than 200 casualties including more than 10 deaths and major economic losses. These cases challenge safety implementation measures of related industries and provide opportunities for research on induced earthquakes.…”
For more than three decades, the depleted Rongchang gas reservoir in China's Sichuan Basin was used for the disposal of unwanted water, which resulted in induced earthquakes, with magnitudes as high as 5.2. After all wells were closed, the frequency of seismic activity was observed to decay following a modified Omori law, and since April 2015, seismic activity again began to increase, and a M4.9 earthquake occurred on 27 December. The results of an epidemic-type aftershock sequence (ETAS) model analysis show that forced seismicity accounted for more than 70% of the total events. For most M ≥ 3.5 earthquakes, including two M ≥ 4 events, the estimated overpressure was lower than the maximum injection pressure. These results, coupled with the fact that postinjection seismic activity has similar characteristics to seismicity during injection, indicate that the injected overpressure fluid was still the driving factor for postinjection seismic activity.
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