Zhao, LiangLiangZhaoAllen, Richard M.Richard M.AllenZheng, TianyuTianyuZhengSHU-HUEI HUNG2019-07-022019-07-022009-09-0100948276https://scholars.lib.ntu.edu.tw/handle/123456789/412277The unusual reactivation of the North China Craton (NCC) challenges the classical views concerning the strength and stability of cratonic lithosphère. By using teleseismic body-waves recorded at 250 seismic stations, this paper presents high-resolution North China Models of P- and S-wave velocity based on finite-frequency kernel tomography. Both P- and S-wave velocity models reveal that: (1) an obvious N-S trending narrow low-velocity region is located at the base of the lithosphère beneath the Central Block (CB) of the NCC, which extends to more than 500 km depth; (2) a region of high-velocity extends to more than 250-300 km depth beneath the Western Block, in contrast to the much shallower high-velocity zones beneath the CB and shallower high-velocities beneath the Eastern Block. These features suggest that warm mantle material with a source at least as deep as the transition zone, possibly a mantle plume, may be responsible for the reactivation of the NCC. The Central Block may have behaved as a sublithospheric corridor for the warm mantle material due to its pre-existing weakness. Copyright 2009 by the American Geophysical Union.journal article10.1029/2009GL0397812-s2.0-71949123520WOS:000269635500006https://api.elsevier.com/content/abstract/scopus_id/71949123520