The M5.9 earthquake that struck 37 km WNW of Linxia Chengguanzhen, China, on December 18, 2023, resulted from reverse faulting at a shallow depth of 10.0 km. This seismic event occurred in an intraplate region on the northern margin of the tectonically active Tibetan Plateau. Historical data indicates that the area has experienced 23 earthquakes of magnitude 5.5 or greater since 1900, with significant fatalities and damage reported from previous events. Current reports confirm that over 100 individuals have died due to the earthquake's impact.
PREREQUISITESSeismologists, disaster response planners, urban developers, and anyone involved in earthquake risk assessment and management in seismically active regions.
The December 18, 2023, M5.9 earthquake in north-central China occurred as a result of reverse faulting at shallow depth. The earthquake occurred on either a north-striking, steeply dipping, reverse fault or a south-southeast striking, shallowing-dipping, reverse fault. The region where the December 18th earthquake occurred is an intraplate (i.e., not at a plate boundary) region located on the northern margin of the Tibetan Plateau. The Tibetan Plateau is a high topographic region north of the Himalaya Mountains that developed in response to ongoing collision between the India and Eurasia plates.
The Tibetan Plateau is tectonically active, and earthquakes are common throughout the region. Within 250 kilometers of today's event, 23 M5.5 and larger earthquakes have occurred since 1900. The largest of these is a M7.7 earthquake in May 1927, to the north that resulted in roughly 40,000 fatalities. The 1927 earthquake resulted in extreme damage in the Gulan-Wuwei area and resulted in damaging landslides. In April 1990, a M6.5 earthquake, immediately preceded by a M6.3 foreshock and followed by a M6.3 aftershock, led to at least 126 fatalities and extensive shaking damage and landslides. Earthquake-related losses in China are common, even for moderate magnitude earthquakes, owing to the proximity of large population centers to shaking, the prevalence of structures that are vulnerable to earthquake shaking, and the occurrence of landslides in steep topography.