2019 Sichuan earthquake

Last updated
2019 Sichuan earthquake
China Sichuan adm location map.svg
Bullseye1.png
Green pog.svg
Yibin
2019 Sichuan earthquake (Sichuan)
UTC  time2019-06-17 14:55:45
ISC  event 615956027
USGS-ANSS ComCat
Local date17 June 2019 (2019-06-17)
Local time22:55
Magnitude5.8 Mw
Depth6 km (4 mi)
Epicenter 28°24′18″N104°57′25″E / 28.405°N 104.957°E / 28.405; 104.957
Type Oblique slip
Areas affected Sichuan, Chongqing
Max. intensity MMI VIII (Severe)
Aftershocks7
Casualties13 dead, >200 injured

An earthquake measuring 5.8 Mw struck the province of Sichuan in China at 22:55 local time (14:55 UTC), 17 June 2019. [1] Changning and Gong counties in Yibin were particularly affected. 13 people died and more than 200 others were injured. [2]

Contents

Tectonic setting

Sichuan lies within the zone of complex tectonics caused by the continuing convergence of the Indian plate with the Eurasian plate. The active faulting in this area relates to the eastward movement of material away from the Tibetan Plateau, which has been uplifted by this collision. The largest structure in the area is the Longmenshan Fault, movement on which was responsible for the M7.9 2008 Sichuan earthquake. [1]

Earthquake

Modified Mercalli intensities in selected locations [1]
MMI LocationsPopulation exposure
MMI VIII (Severe) Changning 57,000
MMI VII (Very strong) Changning, Gong 319,000
MMI VI (Strong) Gao, Xingwen 794,000
MMI V (Moderate) Yibin 3.55 million
MMI IV (Light) Zigong, Luzhou 24.9 million

Based on the focal mechanism the earthquake was a result of oblique-slip faulting, dominantly reverse faulting with a component of strike-slip. [1] Further analysis suggests that the initial movement was on a reverse fault followed by rupture along a shallow strike-slip fault. The reverse fault movement matches well with the known stress field in the area, but the strike-slip fault is less favourably orientated, suggesting the presence of elevated pore pressures due to water injection associated with solution mining of rock salt. [3] Results from the analysis of Interferometric synthetic-aperture radar (InSAR) data indicate that the reverse fault was shallow enough to be intersected by the openhole sections of some of the injection wells. [4]

A number of aftershocks also occurred. [5]

MagnitudeLocationTime (UTC)Depth
5.819 km S of Changning, China2019-06-17 14:55:456.0 km
5.215 km SSW of Changning, China2019-06-17 15:36:0210.0 km
4.78 km SSE of Changning, China2019-06-17 16:29:0810.0 km
4.914 km SSE of Changning, China2019-06-17 16:37:5610.0 km
4.912 km S of Changning, China2019-06-17 21:03:2610.0 km
5.220 km SSE of Changning, China2019-06-17 23:34:3410.0 km
5.3 [6] 13 km S of Changning, China2019-06-22 14:29:5510.0 km
4.9 [7] 7 km SSE of Changning, China2019-06-23 00:28:1810.0 km

Damage

More than 20,000 houses were badly damaged and some roads, communication infrastructure and hydroelectric power plants were also reported to be affected. [8]

There were 13 deaths overall, 9 of them in Changning County and the other 5 in Gongxian County. [2] A further 220 people were reported injured, 6 of them critically and 16 severely. [8]

See also

Related Research Articles

<span class="mw-page-title-main">2002 Hindu Kush earthquakes</span> Earthquakes in northern Afghanistan

The 2002 Hindu Kush earthquakes struck in northern Afghanistan during the month of March. At least 166 people were killed with a very large and intermediate-depth mainshock on March 3. Three weeks later, at least 1,200 were killed during a moderate but shallow event that had a maximum Mercalli intensity of VII. The M7.4 and M6.1 reverse events were focused in the Hindu Kush mountain range area.

In seismology, a supershear earthquake is when the propagation of the rupture along the fault surface occurs at speeds in excess of the seismic shear wave velocity. This causes an effect analogous to a sonic boom.

The 2000 Yunnan earthquake occurred on January 14 at 23:37 UTC, in Yunnan, China. The earthquake killed 7 people, and caused much damage in central Yunnan Province.

The 1995 Antofagasta earthquake occurred on July 30 at 05:11 UTC with a moment magnitude of 8.0 and a maximum Mercalli intensity of VII. The Antofagasta Region in Chile was affected by a moderate tsunami, with three people killed, 58 or 59 injured, and around 600 homeless. Total damage from the earthquake and tsunami amounted to $1.791 million.

An earthquake occurred in southern Mongolia on December 4, 1957, measuring Mw 7.8–8.1 and assigned XII (Extreme) on the Modified Mercalli intensity scale. Surface faulting was observed in the aftermath with peak vertical and horizontal scarp reaching 9 m (30 ft). Because of the extremely sparse population in the area, this event, despite its magnitude, was not catastrophic. However, 30 people died and the towns of Dzun Bogd, Bayan-leg and Baruin Bogd were completely destroyed.

<span class="mw-page-title-main">Surface rupture</span> Offset at ground-level after earthquakes

In seismology, surface rupture is the visible offset of the ground surface when an earthquake rupture along a fault affects the Earth's surface. Surface rupture is opposed by buried rupture, where there is no displacement at ground level. This is a major risk to any structure that is built across a fault zone that may be active, in addition to any risk from ground shaking. Surface rupture entails vertical or horizontal movement, on either side of a ruptured fault. Surface rupture can affect large areas of land.

<span class="mw-page-title-main">Main Himalayan Thrust</span> Geological feature

The Main Himalayan Thrust (MHT) is a décollement under the Himalaya Range. This thrust fault follows a NW-SE strike, reminiscent of an arc, and gently dips about 10 degrees towards the north, beneath the region. It is the largest active continental megathrust fault in the world.

The 2003 Taungdwingyi earthquake struck central Myanmar at midnight, on 21 September with a magnitude of Mwb  6.6.

<span class="mw-page-title-main">Haiyuan Fault</span> Intracontinental strike-slip fault in Tibet

The Haiyuan Fault is a major active intracontinental strike-slip (sinistral) fault in Central Asia.

The 1973 Luhuo earthquake struck near the town of Zhaggo in Garzê Tibetan Autonomous Prefecture of Sichuan Province, China on February 6, 1973, with a magnitude of 7.6 Ms. The earthquake had a maximum intensity of X (Extreme) on the Modified Mercalli intensity scale. It resulted in between 2,175 and 2,204 deaths and a further 2,743 injuries. Serious and widespread destruction occurred in Luhuo County.

On July 18, 2017, an earthquake struck near the Komandorski Islands, east of the Kamchatka Peninsula in the Bering Sea at 11:34 local time. Although there were no casualties from this earthquake, it was notable for a rare characteristic known as supershear, and is one of the few times a large supershear earthquake has been observed. It was preceded by a few foreshocks months earlier, and aftershocks that continued for nearly six months.

The 2021 Maduo earthquake, also known as the 5.22 earthquake struck Madoi County in Qinghai Province, China on 22 May at 02:04 local time. The earthquake had a moment magnitude and surface-wave magnitude of 7.4. Highway bridges, roads and walls collapsed as a result of the earthquake. According to an anonymous source, at least 20 people were killed, 300 were injured, and 13 were missing. Officials stated that there were no deaths but 19 people sustained minor injuries. It was the strongest in China since 2008. It was assigned a maximum intensity of X in Machali, Maduo County on the China seismic intensity scale and Modified Mercalli intensity scale. This earthquake was preceded by another unrelated earthquake that occurred 5 hours earlier in Yunnan.

The 2020 Kashgar earthquake, also known as the Jiashi earthquake occurred on 19 January 2020 at 21:27:56 China Standard Time in Xinjiang Province, China. According to the United States Geological Survey, the earthquake had a moment magnitude of 6.0 and a surface-wave magnitude of 6.4 according to the China Earthquake Network Center. It struck at a shallow depth of 5.6 km according to the USGS while the CENC has the figure at 16 km. Local emergency management agencies said the earthquake damaged more than 1,000 homes and businesses in the nearby populated towns and villages. One person is known to have died while two other children were injured.

<span class="mw-page-title-main">2021 Chignik earthquake</span> 7th largest earthquake in the US

An earthquake occurred off the coast of the Alaska Peninsula on July 28, 2021, at 10:15 p.m. local time. The large megathrust earthquake had a moment magnitude of 8.2 according to the United States Geological Survey (USGS). A tsunami warning was issued by the National Oceanic and Atmospheric Administration (NOAA) but later cancelled. The mainshock was followed by a number of aftershocks, including three that were of magnitude 5.9, 6.1 and 6.9 respectively.

The 1979 Ghaenat earthquakes were a series of large earthquakes in Qaen County, Khorasan province, northeast Iran, near the Afghanistan border. The first mainshock, known as the Korizan earthquake with a surface-wave magnitude (Ms ) of 6.6 and moment magnitude (Mw ) of 6.8, struck on November 14, while the Ms  7.1 or Mw  7.2 Koli-Boniabad earthquake struck on November 27. The two mainshocks were assigned a maximum Modified Mercalli intensity of VIII (Severe) and X (Extreme), respectively. The earthquakes caused extensive damage throughout northeastern Iran, killing an estimated 297 to 440 people and left at least 279 injured.

The 1850 Xichang earthquake rocked Sichuan Province of Qing China on September 12. The earthquake which caused major damage in Xichang county had an estimated moment magnitude of 7.3–7.9 Mw  and a surface wave magnitude of 7.5–7.7 Ms . An estimated 20,650 people died.

The region of Zhili was struck by a major earthquake with an estimated magnitude of 7.5 Ms or 7.4 Mw on June 12, 1830. The epicentre was close to Cixian, which suffered the most severe damage. A total of 7,477 people died as a result of the earthquake.

The 1955 Zheduotang earthquake, also known as the Kangding earthquake occurred on April 14 at 09:29:02 local time near the city of Kangding in the Garzê Tibetan Autonomous Prefecture, Sichuan. The earthquake had a moment magnitude of 7.0 and a surface wave magnitude of 7.1 and struck at a depth of 10 km. Severe damage occurred in Kangding with the loss of 70 lives.

The 2003 Dayao earthquake occurred on July 21, at 23:16:33 CST. The epicenter of the moment magnitude 5.9 earthquake was in Dayao County in the mountainous area of central Yunnan, China. At least 19 people were killed, 644 were injured, and 8,406 families became homeless. The quake also caused $75 million USD in damage.

References

  1. 1 2 3 4 ANSS. "Sichuan 2019: M 5.8 – 19 km S of Changning, China". Comprehensive Catalog. U.S. Geological Survey. Retrieved 18 June 2019.
  2. 1 2 China Plus (18 June 2019). "Death toll from Sichuan earthquake rises to 13" . Retrieved 18 June 2019.
  3. Liu, Junqing; Zahradník, Jiří (14 February 2020). "The 2019 MW 5.7 Changning Earthquake, Sichuan Basin, China: A Shallow Doublet With Different Faulting Styles". Geophysical Research Letters. 47 (4): e85408. Bibcode:2020GeoRL..4785408L. doi:10.1029/2019GL085408. S2CID   211189096.
  4. Wang, S.; Jiang, G.; Weingarten, M.; Niu, Y. (2020). "InSAR Evidence Indicates a Link Between Fluid Injection for Salt Mining and the 2019 Changning (China) Earthquake Sequence". Geophysical Research Letters. 47 (4): e87603. Bibcode:2020GeoRL..4787603W. doi:10.1029/2020GL087603. S2CID   225224563.
  5. "Latest Earthquakes". United States Geological Survey.
  6. "M 5.3 – 11 km SE of Xunchang, China". United States Geological Survey. Archived from the original on 23 June 2019. Retrieved 19 October 2019.
  7. "M 4.9 – 11 km SSW of Changning, China". United States Geological Survey. Archived from the original on 23 June 2019. Retrieved 19 October 2019.
  8. 1 2 China Plus (19 June 2019). "Relief efforts underway after China quake kills 13, injures 220" . Retrieved 19 June 2019.

The International Seismological Centre has a bibliography and/or authoritative data for this event.