1977 Naghan earthquake
1977 Naghan earthquake is located in Iran
Tehran
Tehran
1977 Naghan earthquake
UTC time1977-04-06 13:36:37
ISC event699473
USGS-ANSSComCat
Local dateApril 6, 1977 (1977-04-06)
Magnitude6.0 Mw
Depth15 km (9.3 mi)
Epicenter31°50′42″N 50°42′40″E / 31.845°N 50.711°E / 31.845; 50.711[1]
TypeReverse
Areas affectedIran
Max. intensityVIII (Severe)
Casualties348–366 killed

The 1977 Naghan earthquake struck Chaharmahal and Bakhtiari province in Iran on April 6 at 13:36 UTC. The earthquake measuring 6.0 Mw  occurred at a depth of 15 km (9.3 mi) and had a maximum Modified Mercalli intensity of VIII (Severe).[2] More than 2,100 homes were destroyed and at least 348 people (some sources say 366) were killed.[3]

Tectonic setting

Iran is a region that accommodates oblique convergence through thrust and strike-slip faults with clear geomorphic expression at the surface. These pure thrust and pure strike-slip faults run parallel to each other. Beginning in the Miocene or Cenozoic, continental collision involving the Arabian Plate and Central Iran formed the 1,200 km (750 mi)-long Zagros Mountains. The mountain belt trends northwest–southeast from Eastern Anatolia to the Strait of Hormuz. Approximately 30–50 percent of the ~25 cm (9.8 in)/yr convergence between the Arabian and Eurasian plates is accommodated along the Zagros.[4]

Earthquake

Major faults in this zone include the Main Zagros Reverse Fault (MZRF) which is an inactive thrust fault bounding the northern Zagros. This fault was active when subduction was ongoing. The fault became inactive when suturing occurred and continental collision began. The Kazerun—Borazjan Fault (KBF) system is another major structure, consisting of a wide zone of right-lateral faults that cuts through the belt. It lies in the middle of the belt. To the east, the Zagros fold and thrust zone accommodates convergence through thrust and strike-slip faulting. Strike-slip faulting is mainly accommodated along the northwest–southeast trending Main Recent Fault which displays right-lateral displacement. The fault is parallel to the MZRF and mountain belt. The KBF fault accommodate the different rate of convergence between the northwestern and southeastern belt. It consists of three segments—the Dena, Kazerun, and Borazjan faults. At its southern extent, these fault segments curve to the east and display reverse faulting. The northern KBF meets the Main Recent Fault (Ardal Fault segment) near Borujen where it also accommodates strike-slip deformation. The MRF also runs parallel to the belt.[4]

Seismicity on the Ardal Fault is high—earthquakes were recorded near the fault in 1666, 1874 and 1880. Along the Dena Fault, earthquakes were recorded in 1934, 1975 and 1989. The earthquake on April 6, 1977 occurred near the Ardal Fault. It displayed a both reverse and strike-slip focal mechanism but no surface ruptures were identified. The fault plane was identified as trending west-northwest–east-southeast. A focal depth of 6 km (3.7 mi) was calculated. The reverse focal mechanism is inconsistent with rupture on the Dena Fault and suggest it was produced on the Dopolan or the Gazulak faults. These north–northeast dipping reverse faults produce surface expressions further south of the epicenter.[4]

Damage

Destruction occurred over a 150 km2 (58 sq mi) area where 384 people and 0.7 percent of the region's livestock perished. A further 200 were injured. The most recorded number of deaths was at Naghan, where 202 died. There were 43 and 64 fatalities at Jaghdan and Ardal, respectively. At Dastgerd, 11 were killed. More than 2,100 homes were destroyed or damaged beyond repair. Eight schools were total losses while another 37 were damaged. The earthquake occurred during a period of heavy rainfall. This furthered the destruction in areas on alluvium with high clay saturation. Landslides occurred on the steem mountain slopes, affecting villages. There was additional damage from the aftershocks.[5]

Adobe brick and masonry buildings made up 90 percent of houses in the region. Most adobe brick houses were razed or damage to the extent that they were unsafe for use. The walls of these homes consisted of adobe-brick and clay mortar, as well as heavy wooden beams and clay which served as roofs. These materials were not resistant to seismic shaking, leading to destruction. Many deaths were associated with these structure collapses. In Jaghdan, all adobe brick homes were lost. Masonry construction were also affected—one school in Ardal was partially destroyed.[5]

See also

References

  1. ↑ ISC (27 June 2022), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009), Version 9.1, International Seismological Centre
  2. ↑ ANSS, "M 5.9 - 32 km SSE of Fārsān, Iran 1977", Comprehensive Catalog, U.S. Geological Survey
  3. ↑ National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Database (Data Set), National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K
  4. 1 2 3 Yamini-Fard, F.; Hatzfeld, D.; Tatar, M.; Mokhtari, M. (2006). "Microearthquake seismicity at the intersection between the Kazerun fault and the Main Recent Fault (Zagros, Iran)". Geophysical Journal International. 166 (1): 186–196. Bibcode:2006GeoJI.166..186Y. doi:10.1111/j.1365-246X.2006.02891.x. S2CID 130787307.
  5. 1 2 Berberian, M.; Navai, I. (1978). "Naghan (Chahar Mahal Bakhtiari-High Zagros, Iran) Earthquake of 6 april 1977. A preliminary field report and a seismotectonic discussion". Annals of Geophysics. 31 (1): 5–27. doi:10.4401/ag-4741. S2CID 126620209.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.