Mapping heterogeneity of the uppermost inner core using two pairs of core phases

被引:17
作者
Kaneshima, S
机构
[1] Geology Department, University of Bristol, Wills Memorial Building, Bristol BS8 1RJ, Queens Road
[2] Dept. of Earth and Planetary Physics, Faculty of Sciences, Tokyo University
关键词
DIFFERENTIAL TRAVEL-TIMES; OUTER CORE; ANISOTROPY; BOUNDARY; WAVE; PKP; MANTLE; CONSTRAINTS; PKIKP; MODEL;
D O I
10.1029/96GL03026
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Two pairs of core phases, PKPcd-PKPdf and PKPbc-PKPdf, are analysed to map the P-wave velocity (Vp) of the uppermost inner core. Waveform analysis of PKPcd-PKPdf shows that Vp relative to PREM (delta Vp) within 100 km from the inner core boundary (ICB) is laterally heterogeneous by -0.5% to +0.1% with a wavelength of nearly 1000 km. Differential travel times of PKPbc-PKPdf relative to PREM (delta Tbc-df) are positive (negative) for the regions of positive (negative) delta Vp near the ICB. This correlation indicates that the lateral Vp variation exists predominantly in the inner core side of the ICB. Absolute values of delta Tbc-df for both positive and negative delta Vp regions are too large to be explained with models in which lateral delta Vp variation is restricted within the upper 200 km of the inner core. The lateral variation appears to extend at least to 300 km below the ICB.
引用
收藏
页码:3075 / 3078
页数:4
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