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Reactivation of an Archean craton: Constraints from P‐ and S‐wave tomography in North China
Author(s) -
Zhao Liang,
Allen Richard M.,
Zheng Tianyu,
Hung ShuHuei
Publication year - 2009
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2009gl039781
Subject(s) - craton , geology , lithosphere , mantle (geology) , archean , seismology , transition zone , mantle plume , seismic tomography , plume , low velocity zone , geophysics , tectonics , paleontology , physics , meteorology
The unusual reactivation of the North China Craton (NCC) challenges the classical views concerning the strength and stability of cratonic lithosphere. 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 lithosphere 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.