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Mid‐lithosphere discontinuities beneath the western and central North China Craton
Author(s) -
Sun Weijia,
Kennett B. L. N.
Publication year - 2017
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 - 10.1002/2016gl071840
Subject(s) - lithosphere , craton , geology , classification of discontinuities , seismology , discontinuity (linguistics) , tectonics , geophysics , seismic tomography , seismic array , mantle (geology) , mathematical analysis , mathematics
By analyzing P reflectivity extracted from stacked autocorrelograms for teleseismic events on a dense seismic profile, we obtain a detailed image of the mid‐lithosphere discontinuity (MLD) beneath western and central North China Craton (NCC). This seismic daylight imaging exploits a broad high‐frequency band (0.5–4 Hz) to reveal the fine‐scale component of multi‐scale lithospheric heterogeneity. The depth of the MLD beneath the western and central parts of the NCC ranges 80–120 km, with a good match to the transition to negative S velocity gradient with depth from Rayleigh wave tomography. The MLD inferred from seismic daylight imaging also has good correspondence with the transition from conductive to convective regimes estimated from heat flow data indicating likely thermal control within the seismological lithosphere.