Induced or triggered? The deadly February 2019 Rongxian-Weiyuan ML 4.9 earthquake in the shale gas field in Sichuan, China Article Swipe
Hongfeng Yang
,
Pengcheng Zhou
,
Nan Fang
,
Gaohua Zhu
,
Wenbin Xu
,
Jinrong Su
,
Fanbao Meng
,
Risheng Chu
·
YOU?
·
· 2020
· Open Access
·
· DOI: https://doi.org/10.5194/egusphere-egu2020-12096
YOU?
·
· 2020
· Open Access
·
· DOI: https://doi.org/10.5194/egusphere-egu2020-12096
<p>Coinciding with the extensive hydraulic fracturing activities in the southern Sichuan basin, seismicity in the region has surged in the past a few years, including a number of earthquakes with magnitudes larger than 5. On 25 February 2019, an M<sub>L</sub>4.9 earthquake struck the Rongxian County, Sichuan, China and caused 2 fatalities and 12 injuries, the first deadly earthquake associated with shale gas production. The earthquake was preceded by two foreshocks with magnitudes of M<sub>L</sub>4.7 and M<sub>L</sub>4.3 within two days. We relocated the earthquake sequence using local and regional seismic network, and obtained the focal depths of the mainshock and two foreshocks at 1 and 3 km, respectively, much shallower than the report from catalogue. Most other smaller quakes were located at 2-6 km. The mainshock had also been well captured by InSAR images, which confirmed the shallow depth of ~1 km. Both seismic and geodetic data yielded thrust faulting mechanism for the mainshock, consistent with the mapped Molin fault in the region. The two foreshocks, however, occurred on an unmapped fault that has different orientation than the Molin fault. Injection wells are found in the vicinity of the two foreshocks and the fracking depth (~2.7 km) coincides with their focal depths, suggesting a possible causal relationship. The mainshock is located in the region with positive Coulomb failure stress caused the two foreshocks. The value of Coulomb failure stress change is 0.03 bar, smaller than the typical static triggering threshold. Therefore, the mainshock is likely caused by fracking by poroelastic stress transfer.</p>
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- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.5194/egusphere-egu2020-12096
- OA Status
- gold
- Cited By
- 1
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All OpenAlex metadata
Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W3091849197Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.5194/egusphere-egu2020-12096Digital Object Identifier
- Title
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Induced or triggered? The deadly February 2019 Rongxian-Weiyuan ML 4.9 earthquake in the shale gas field in Sichuan, ChinaWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2020Year of publication
- Publication date
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2020-03-09Full publication date if available
- Authors
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Hongfeng Yang, Pengcheng Zhou, Nan Fang, Gaohua Zhu, Wenbin Xu, Jinrong Su, Fanbao Meng, Risheng ChuList of authors in order
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https://doi.org/10.5194/egusphere-egu2020-12096Publisher landing page
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YesWhether a free full text is available
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goldOpen access status per OpenAlex
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https://doi.org/10.5194/egusphere-egu2020-12096Direct OA link when available
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Foreshock, Geology, Seismology, Fault (geology), Induced seismicity, AftershockTop concepts (fields/topics) attached by OpenAlex
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1Total citation count in OpenAlex
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| abstract_inverted_index.vicinity | 185 |
| abstract_inverted_index.Injection | 179 |
| abstract_inverted_index.coincides | 196 |
| abstract_inverted_index.confirmed | 134 |
| abstract_inverted_index.different | 173 |
| abstract_inverted_index.extensive | 3 |
| abstract_inverted_index.hydraulic | 4 |
| abstract_inverted_index.including | 24 |
| abstract_inverted_index.injuries, | 53 |
| abstract_inverted_index.mainshock | 97, 124, 207, 241 |
| abstract_inverted_index.mechanism | 149 |
| abstract_inverted_index.relocated | 80 |
| abstract_inverted_index.shallower | 108 |
| abstract_inverted_index.Therefore, | 239 |
| abstract_inverted_index.activities | 6 |
| abstract_inverted_index.associated | 58 |
| abstract_inverted_index.catalogue. | 113 |
| abstract_inverted_index.consistent | 153 |
| abstract_inverted_index.earthquake | 40, 57, 64, 82 |
| abstract_inverted_index.fatalities | 50 |
| abstract_inverted_index.foreshocks | 69, 100, 189 |
| abstract_inverted_index.fracturing | 5 |
| abstract_inverted_index.magnitudes | 30, 71 |
| abstract_inverted_index.mainshock, | 152 |
| abstract_inverted_index.seismicity | 12 |
| abstract_inverted_index.suggesting | 201 |
| abstract_inverted_index.threshold. | 238 |
| abstract_inverted_index.triggering | 237 |
| abstract_inverted_index.earthquakes | 28 |
| abstract_inverted_index.foreshocks, | 164 |
| abstract_inverted_index.foreshocks. | 221 |
| abstract_inverted_index.orientation | 174 |
| abstract_inverted_index.poroelastic | 248 |
| abstract_inverted_index.production. | 62 |
| abstract_inverted_index.relationship. | 205 |
| abstract_inverted_index.respectively, | 106 |
| abstract_inverted_index.&lt;p&gt;Coinciding | 0 |
| abstract_inverted_index.transfer.&lt;/p&gt; | 250 |
| abstract_inverted_index.M&lt;sub&gt;L&lt;/sub&gt;4.3 | 75 |
| abstract_inverted_index.M&lt;sub&gt;L&lt;/sub&gt;4.7 | 73 |
| abstract_inverted_index.M&lt;sub&gt;L&lt;/sub&gt;4.9 | 39 |
| cited_by_percentile_year.max | 94 |
| cited_by_percentile_year.min | 89 |
| countries_distinct_count | 1 |
| institutions_distinct_count | 8 |
| citation_normalized_percentile.value | 0.52688013 |
| citation_normalized_percentile.is_in_top_1_percent | False |
| citation_normalized_percentile.is_in_top_10_percent | False |