Physics
Scientific paper
Oct 2010
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010georl..3719307w&link_type=abstract
Geophysical Research Letters, Volume 37, Issue 19, CiteID L19307
Physics
2
Seismology: Seismicity And Tectonics (1207, 1217, 1240, 1242), Seismology: Continental Crust (1219), Seismology: Lithosphere (1236), Tectonophysics: Continental Contractional Orogenic Belts And Inversion Tectonics, Tectonophysics: Rheology: Crust And Lithosphere (8031)
Scientific paper
A total of 400 regional earthquakes were located in northern Tibetan Plateau from data recorded by INDEPTH-IV and PKU Eastern Kunlun arrays from May 2007 to June 2009. The distribution of these earthquakes is compatible with a continuously deforming Tibetan lithosphere. Most earthquakes occur at a depth range of 0-15 km, but no event is deeper than 30 km. This observation strongly supports the existence of a hot and weak lower crust beneath the northern Tibet. The crustal seismogenic zone appears slightly thicker beneath the northern Tibet than in the southern plateau, possibly reflecting a difference in the rheological (dry vs. wet) structure of the crust. The absence of lower crustal and uppermost mantle earthquakes in northern Tibet is consistent with a localized asthenospheric upwelling under the Qiangtang and Songpan-Ganze terranes. Finally, the lack of mantle earthquakes should be fully addressed in any models of subduction in northern Tibet.
Chen Yongshun John
Fan Wenyuan
Feng Yongge
Ge Zengxi
Hearn Thomas M.
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