Crustal structure of Hubei Province of China from teleseismic receiver functions: Evidence for lower crust delamination
Western Hubei Province is at the southern end of the 3000-km-long north-south-oriented Xing'anling–Taihangshan–Wulingshan topographic step in China, which separates high-rising plateaus and mountain ranges in the west from low-elevation plains in the east. We calculated teleseismic P receiver f...
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Veröffentlicht in: | Tectonophysics 2014-12, Vol.636, p.286-292 |
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