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The Shanxi Rift System or Fen–Wei Rift System [1] is a zone of active extensional tectonics that forms the eastern margin of the Ordos Block in northern China. The zone extends for at least 900 km (560 mi) and runs south-southwest to north-northeast.
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17 lut 2021 · The Shanxi Rift System (SRS) is a prominent intracontinental rift in eastern Eurasia. However, its tectonic origin remains enigmatic, as the timing of rift initiation and its subsequent evolution is not well constrained.
Download scientific diagram | Map of the Shanxi Rift, Taihangshan, and eastern Ordos block showing principal range‐bounding faults and locations of published and new AFT data discussed in the...
Shanxi Great Rift Valley, a miraculous work of nature, extends for tens of miles and has a vertical section of 10 kilometers. How did it originate? #naturelo...
24 paź 2020 · In order to study continental rifting mechanism, intraplate volcanism, and seismicity of the Shanxi Rift, we construct a high-resolution 3-D lithospheric shear velocity (Vs) model with a focus of the crust by jointly inverting Rayleigh wave dispersion curves and ellipticity measurements.
