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Chen, Wang-Ping Yang, Zhaohui 2015-09-28T15:12:33Z 2015-09-28T15:12:33Z 10000-01-01 2009 2009 Additional evidence for this conclusion comes from my study of eleven intracontinental earthquakes, with magnitudes ranging from 4.9 to 6, which occurred in the mantle beneath the western Himalayan syntaxis, the western Kunlun Mountains, and southern Tibet (near Xigaze). High-resolution seismic waveforms show that some focal depths exceeded 100 km, indicating that these earthquakes also occurred in the mantle lithosphere, even though the crust has been greatly thickened. Made available in DSpace on 2015-09-28T15:12:33Z (GMT). No. of bitstreams: 2 license.txt: 4848 bytes, checksum: 96035ab3f5e1c23cc7138a224ce498bd (MD5) 3363121.pdf: 3112332 bytes, checksum: 2b436c1816a2f0f25e35fa47e2c9af18 (MD5) Previous issue date: 2009 Embargo set by: Seth Robbins for item 87823 Lift date: Forever Reason: Restricted to the U of I community idenfinitely during batch ingest of legacy ETDs Restricted to the U of I community idenfinitely during batch ingest of legacy ETDs U of I Only 145 p. Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 2009. http://hdl.handle.net/2142/86542 (MiAaPQ)AAI3363121 eng Geology Seismic Studies of the East African Rift System and the Tibetan Plateau: Implications for the Rheology of Lithosphere and the Evolution of Rifts in Continents text Geology Geology University of Illinois at Urbana-Champaign Dissertation Ph.D.