Beijing Anomaly

The Beijing Anomaly is an observed seismic feature in the Earth's mantle at a depth of around 700–1400 km below Northeastern China where a high degree of seismic attenuation was discovered to exist. According to its discoverers, Jesse Lawrence (from Scripps Institution of Oceanography) and Michael Wysession (from Washington University in St.

Source: Wikipedia — Beijing Anomaly (CC BY-SA 4.0)

Beijing Anomaly

The Beijing Anomaly is an observed seismic feature in the Earth's mantle at a depth of around 700–1400 km below Northeastern China where a high degree of seismic attenuation was discovered to exist. According to its discoverers, Jesse Lawrence (from Scripps Institution of Oceanography) and Michael Wysession (from Washington University in St.

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Source: Wikipedia "Beijing Anomaly" · CC BY-SA 4.0

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