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Dissimilarity of the Earth's Inner Core Surface Under South America and Northeastern Asia Revealed by Core Reflected Phases
Author(s) -
Krasnoshchekov Dmitry,
Ovtchinnikov Vladimir,
Polishchuk Valentin
Publication year - 2019
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.983
H-Index - 232
eISSN - 2169-9356
pISSN - 2169-9313
DOI - 10.1029/2019jb017408
Subject(s) - inner core , inner mongolia , outer core , geology , mantle (geology) , core (optical fiber) , amplitude , jump , boundary (topology) , china , geodesy , geography , geophysics , physics , optics , astronomy , mathematics , mathematical analysis , archaeology
Resolving topography of the inner core boundary (ICB) and the structure and composition of the nearby region is key to improving our understanding of solidification of the Earth's inner core. Observations of travel times and amplitudes of short‐period seismic phases of PKiKP and PcP reflected, respectively, off the inner and outer boundary of the liquid core, provide essential constraints on the properties of this region. We revisit heterogeneities of ICB using a total of more than 1,300 new differential travel times and amplitude ratios of PKiKP and PcP measured at 3.2–35.2° and reflected off the core's boundaries under Northeastern Asia and South America. We observe a statistically significant systematic bias between the measurements collected in the two spots. We carefully examine its origin in terms of contributions by various Earth's shells and find that most of variance in PKiKP‐PcP differential travel times measured above the epicentral distance of 16.5° in Northeastern Asia can be accounted for by mantle corrections. We find slight disparity of about 1–3 km between the outer core thickness under Asia and America; the ICB density jump under Northeastern Asia is about 0.3 g/cm 3 , which is three times as small as under South America. The findings are interpretable either as evidence for inner core hemispherical asymmetry, whereby crystallization dominates in the West and melting in the East (not vice versa), or in terms of two disconnected mosaic patches with contrasting properties.