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The earthquake occurred as a result of shallow (10 km depth) strike-slip faulting at the northeastern Tibetan Plateau. It ruptured a fault located near the Qilian Mountains. The geological structure responsible was the Lenglongling Fault, a segment of the Haiyuan Fault System. The rupture was mostly confined to 0–8 km within the upper crust.
In the region of the April 13 earthquake the Tibetan Plateau is extending and translating east-southeastward within a larger zone of generally north–south convergence. [3] Based on the location, depth, and moment tensor of the event, the Qinghai Province earthquake likely reflects the interplay amongst these major tectonic forces, dominated ...
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The death toll from China’s most powerful earthquake in years has risen to 149, with two people still missing after the tremor hit northwestern parts of the country last week. The 6.2-magnitude ...
Together with 198 in Qinghai, that brought the total injured close to 1,000. Villagers in Yangwa bundled up against the cold and ate instant noodle soup being served in a tent of translucent green ...
The magnitude of this earthquake has been calculated from observations of surface rupture and estimates of co-seismic (during the earthquake) slip. A total of about 100 km of rupture have been mapped on the Dangjiang fault segment. A maximum left-lateral offset of 3.3 m has been measured and an average offset of 2.2 m.
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The earthquake occurred in a Tibetan region in Qinghai province, where 93% of the local population is of Tibetan ethnicity, and many locals do not speak or understand Mandarin Chinese, and the community was home to large numbers of Tibetan Buddhists.