2020 Kashgar earthquake

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2020 Kashgar earthquake
China Xinjiang Southern relief location map.svg
Bullseye1.png
UTC  time2020-01-19 13:27:56
ISC  event 617194918
USGS-ANSS ComCat
Local dateJanuary 19, 2020 (2020-01-19)
Magnitude6.0 Mw [1]
6.4 Ms [2]
Depth5.6 km (3.5 mi)
Epicenter 39°50′06″N77°06′29″E / 39.835°N 77.108°E / 39.835; 77.108
TypeReverse
Areas affected Xinjiang, China
Max. intensity VIII (Severe) [1]
CSIS VIII [3]
Casualties1 dead, 2 injured [4]

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. [1] [5] 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. [6] [1]

Contents

Tectonic setting

Northern Xinjiang lies at the northernmost extreme zone of continental deformation as a result of the ongoing collision between India and Eurasia. The epicenter region of the 2020 Kashgar earthquake lies along the Kalpin (Kepingtage or Kalpingtag) fold and thrust belt, which has folded and uplifted strata to form the Chinese Tian Shan mountains. [7] This fold and thrust belt is located at the southern foot of the Chinese Tien Shan range and is 300 km long while being 75 km wide. It consists of a series of anticlines, three low-angle thrust faults and an underlying décollement. [7] These faults and the décollement aid in the subduction of the Tarim basin.

The fold and thrust belt is seismically active and is the source of many moderately large to major events with focal depths of between 15 km to 32 km. [8] Historically, the region has hosted many large magnitude 6.0+ earthquakes, but their destructive capabilities were limited due to the sparse population density. The largest event ever recorded was the 1902 Turkestan earthquake, with an estimated moment magnitude of 7.7. [9] It had an epicenter very close to that of the 2020 event and is thought to have ruptured the decollément. This earthquake killed anywhere between 5,000 and 20,000 people in nearby Kashgar. Another earthquake in 1996 resulted in the death of at least 24 individuals and damaged more than 15,300 homes. [10] The magnitude 6.3 earthquake in 2003 has an epicenter just south of where the 2020 earthquake was. It killed some 216 people and left 4,000 injured. It also collapsed more than 71,000 and damaged at least 41,000 others. [11]

The slip rate along the shallow frontal part of the Kalping fold and thrust belt has been measured at 1 to 2 mm/yr or just one-fourth the rate of subduction of the Tarim basin. This differs from most zones of convergence where the outermost thrust results in the greatest deformation and accommodates the most slip. Because much of the geological deformation and activity is not at the outer thrusts, the faults are moving at much slower rates. While the faults of the Kalping fold and thrust belt are active and seismogenic, much of the décollement is not due to the lack of friction. It instead displays aseismic creep at depth. [12]

Earthquake

According to the United States Geological Survey, the earthquake ruptured with a shallow focal depth of 5.6 km at the foothills of the Tien Shan mountains. The epicenter of the earthquake is located in close proximity to the G3012 Turpan–Hotan Expressway, or 104 km east northeast of the city of Kashgar. [1]

The China Earthquake Network Center stated that the earthquake registered 6.4 Ms on the Chinese surface wave magnitude scale. A hypocenter depth of 16 km was estimated. [5]

The mainshock was followed by a number of aftershocks, the largest measuring Mw 5.0 or Ms 5.2. [13] According to the China Earthquake Administration, ten aftershocks were measured with magnitudes greater than 3.0, in the range of 4.3 to 5.0. [14] A strong Mw 5.3 foreshock occurred on January 17 with an epicenter south southeast of the mainshock epicenter. [15]

Characteristics

Focal mechanism solutions provided by the USGS show that the earthquake occurred as the result of shallow reverse faulting, with a small strike-slip component. [16] Source models using InSAR data show the earthquake involved slippage on the flat portion of a listric fault without rupturing to the surface. Rupture geometry reveals a 34 km by 12 km zone of slip on the fault at a depth of between 5–7 km. The maximum slip caused by the earthquake is estimated to be 0.29 meters at a depth of 6.3 km. The epicenter of this earthquake is said to have been at the southern margin of the Kalpin fold and thrust belt, where the Tian Shan meets the Tarim basin. Calculating the Coulomb stress transfer caused by the earthquake demonstrates the increased risk of seismic hazard in the region. With the lack of aftershocks and the pattern of historic seismicity in the region, another large earthquake may occur in the future. [12]

A more recent analysis of the event reveals that this occurred beneath the shallow décollement, consistent with earlier earthquakes in 1997, 1998, and 2003. [16] By relocating the hypocenter, a different focal depth was found, 15–18 km beneath the fold and thrust belt. It is thought to involve a rupture on a much deeper and older fault structure. [16]

Impact

A USGS ShakeMap of the Mw6.0 earthquake in Xinjiang. M 6.0 - 86km ENE of Arzak, China - ShakeMap.jpg
A USGS ShakeMap of the Mw6.0 earthquake in Xinjiang.

The earthquake had a maximum intensity of VIII on the Mercalli intensity scale and China seismic intensity scale. [5] [1] According to a local villager in Guleruk Township, Jiashi County who survived the earthquake, it was described as violent and "like thunder", adding that the shaking lasted for 20 to 30 seconds.

One person was seriously injured and was reported deceased later. [17] Local media then reported that "many" people also sustained light injuries due to the earthquake. This claim was later specified to just two individuals suffering minor injuries and one person dying. [18] The Xinjiang Railway Department immediately suspended 9 passenger trains from operating in the affected area. [19]

Local emergency workers inspected some 206 homes and found eight total collapses, 122 with collapsed walls and 68 with partially cracked or fallen walls. [20] Four self-constructed shops totally collapsed in the earthquake and 52 other homes had moderate damage. Another 955 homes sustained light damage. A 1.1 km and 5.6 km-long wall also collapsed due to the quake. Roads including a major highway and transmission lines were severely compromised by the temblor as well.

See also

Related Research Articles

<span class="mw-page-title-main">Payzawat County</span> County in Xinjiang, China

Payzawat County, also via SASM/GNC romanization as Payziwat County, and via Mandarin Chinese as Jiashi County is a county in Kashgar Prefecture, Xinjiang Uyghur Autonomous Region, China, on the western rim of the Taklamakan Desert. To the east, the county borders Maralbexi County, to the south Yopurga County.

The 2003 Bachu earthquake occurred on 24 February at 10:03 local time in the Xinjiang Autonomous Region in northwest China. The epicentre was located near to the town of Jiashi and Bachu County, approximately 105 km east of Kashgar and 310 km west of Aksu.

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The Jiashi earthquakes were a series of earthquakes from 1997 to 2003, with several earthquakes larger than Ms 6 occurring between January and April, 1997. Two strong earthquakes with magnitudes Ms  6.4 and 6.3 occurred on January 21, 1997, at 09:47 and 09:48 local time, respectively, in Jiashi County of Xinjiang Autonomous Region, NW China. The earthquakes occurred on a major strike-slip fault beneath the Tarim Basin. The fault has no surface expression and prior to the earthquake was unknown. At least 12 people were killed and 40 injured in the earthquakes of January 21. Another earthquake on March 1, 1997, at 14:04 local time with magnitude Ms  6.0 killed another person. On April 6, 11 and 16, other four earthquakes with magnitudes Ms  6.3, 6.4, 6.6 and 6.3 killed 8 people. Several predictions were made in this earthquake series. Some of the predictions were not fulfilled, while some preceded the predicted earthquake from 2.5 hours to 4 days. The April 11 earthquake occurred 30 minutes after a prediction was made. Rebiya Kadeer wrote that her career was significantly affected by the earthquakes, which were "one of the worst natural disasters that had occurred in the Uyghur nation in recent memory." One hundred villages and one thousand homes were leveled. Kadeer organized donations and aid for the area.

A potent magnitude 6.6 Mw intraplate aftershock occurred at 17:16 JST (08:16 UTC) on 11 April, in the Hamadōri region of Fukushima, Japan. With a shallow focus of 13 km (8.1 mi), the earthquake was centred inland about 36 km (22 mi) west of Iwaki, causing widespread strong to locally severe shaking. It was one of many aftershocks to follow the 11 March Tōhoku earthquake, and the strongest to have its epicentre located inland.

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On December 7, 2015, an earthquake measuring 7.2 on the moment magnitude scale struck Tajikistan 105 km (65 mi) west of Murghab at 07:50 UTC at a depth of 26.0 km (16.2 mi). The earthquake was also felt in neighboring Xinjiang in China, India, Afghanistan, Pakistan and Kyrgyzstan.

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The 1902 Turkestan earthquake devastated Xinjiang, China, near the Kyrgyzstan border. It occurred on August 22, 1902, at about 8:00 or 9:00 am local time with an epicenter near the Tien Shan mountains. The thrust earthquake measured 7.7 on the moment magnitude scale (Mw ) and had a depth of 18 km (11 mi).

The 1906 Manasi earthquake (玛纳斯地震), also known as the Manas earthquake occurred in the morning of December 23, 1906, at 02:21 UTC+8:00 local time or December 22, 18:21 UTC. It measured 8.0–8.3 on the moment magnitude scale and 8.3 on the surface-wave magnitude scale. The epicenter of this earthquake is located in Manas County, Xinjiang, China. An estimated 280–300 people died and another 1,000 more were injured by the earthquake.

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The 1995 Menglian earthquake or 1995 Myanmar–China earthquake occurred on 12 July at 05:46:43 local time in the Myanmar–China border region. The earthquake had an epicenter on the Myanmar side of the border, located in the mountainous region of Shan State. It registered 7.3 on the Chinese surface wave magnitude scale (Ms ) and 6.8 on the moment magnitude scale (Mw ). With a maximum Mercalli intensity assigned at VIII, the quake killed eleven people and left another 136 injured. Over 100,000 homes in both countries were destroyed and 42,000 seriously damaged. Some damage to structures were also reported in Chiang Mai and Chiang Rai, Thailand. The low death toll from this earthquake was attributed to an early warning issued prior to it happening. Precursor events including foreshocks and some seismic anomalies led to an evacuation of the area before the mainshock struck. It is thought to be one of the few successfully predicted earthquakes in history.

The 1889 Chilik earthquake occurred on July 11 on the Gregorian calendar, or June 30 on the Julian calendar at 15:14 local time in the Tien Shan mountains. The earthquake measured an estimated Mw  7.9–8.0 on the moment magnitude scale and was assigned a maximum intensity of X (Devastating) on the MSK 64 and Rossi-Forel scales. Over 92 people across Kazakhstan, Kyrgyzstan and China were killed.

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The 1998 Zhangbei–Shangyi earthquake occurred at 11:50 local time on 10 January with a moment magnitude of 5.7 at a depth of 14.1 km. It struck the province of Hebei in Zhangjiakou. At least 70 people died, 11,500 were injured and a further 44,000 families were homeless in the wake of the event. Damage was reported in the town of Zhangbei, Hebei Province, as well as to sections of the Great Wall of China.

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