1977 San Juan earthquake

Tectonic setting

San Juan Province lies in an area where the South American plate is affected by flat-slab subduction of the underlying Nazca plate, the so-called Pampean flat-slab. The very shallow angle leads to a much greater degree of coupling between the subducting and overriding plates. The increased coupling leads to shortening of the crust of the South American plate, causing active thrust tectonics and rapid uplift, forming the Sierras Pampeanas. The Pie de Palo range is one of the active structures, interpreted to be controlled by major thrust faults. The overall structure has been interpreted as both thin-skinned and thick-skinned.

Earthquake

The earthquake consisted of two sub-events, separated by about 20 seconds, treated by some seismologists as foreshock and mainshock. The observed focal mechanism was reverse faulting, on a north–south trending structure. From the mainshock alone, it was not possible to decide whether the fault responsible dipped to the west or east. Analysis of the aftershock sequence suggests that two separate faults moved during the earthquake, the earlier event on a segment to the north and the later one to the south. The fault segments have been interpreted as both alternating west and eastward-dipping faults or as an east-dipping fault in the hanging-wall of a larger west-dipping fault.

There was no surface rupture associated with the earthquake and it is an example of a blind thrust earthquake on thrust faults underlying the Pie de Palo range.

Damage

There was widespread damage in San Juan Province. The towns of Bermejo and Caucete were particularly badly affected. Many houses constructed of adobe or unreinforced masonry were either badly damaged or destroyed and very large areas were affected by liquefaction. More modern structures, built to earthquake resistant designs, in contrast showed little damage. At least 65 people were killed and a further 284 were injured. The extensive damage left many homeless, with estimates in the range 20,000 to 40,000.

The area's wine industry was heavily impacted due to damage to both buildings and particularly wine storage tanks, reducing the wine storage capacity of the affected area by about 10 million litres.

References

References

1. (27 June 2022). "ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009)". [[International Seismological Centre]].
2. (2015). "Active basement uplift of Sierra Pie de Palo (Northwestern Argentina): Rates and inception from ¹⁰Be cosmogenic nuclide concentrations". Tectonics.
3. (1996). "Rupture distribution of the 1977 western Argentina earthquake". Physics of the Earth and Planetary Interiors.
4. (1992). "Seismotectonics of Sierra Pie de Palo, a basement block uplift in the Andean Foreland of Argentina". Bulletin of the Seismological Society of America.
5. (2016). "Crustal shortening at the Sierra Pie de Palo (Sierras Pampeanas, Argentina): near-surface basement folding and thrusting". Geological Magazine.
6. (2010). "Crustal-scale pure shear foreland deformation of western Argentina". Geophysical Research Letters.
7. Rohjan, C.. (1978). "Seismic engineering program report, September-December 1977". U.S. Dept. of the Interior, Geological Survey.
8. (1994). "Liquefaction during the 1977 San Juan Province, Argentina earthquake (M_s = 7.4)". Engineering Geology.
9. National Geophysical Data Center / World Data Service (NGDC/WDS). (1972). "Significant Earthquake Database". [[National Geophysical Data Center]], [[National Oceanic and Atmospheric Administration.
10. Utsu, T. R.. (2002). "International Handbook of Earthquake & Engineering Seismology". [[Academic Press]].