The seismic phase PKiKP, reflected from the inner core, and its coda give information on the short scale heterogeneities at and below the inner core boundary (ICB) of the Earth. We have collected PKiKP recorded at short distances (<45°) at broadband sta
The idea of Earth inner core anisotropy is well-established, and it is a very important topic in und...
Travel times, listed in the I.S.S., of longitudinal waves at distances of 100 " < A < 115...
The structure of the Earth’s inner core is not well known between depths of ∼100–200 km beneath the ...
The seismic phase PKiKP, reflected from the inner core, and its coda give information on the short s...
The hemispherical pattern of seismic velocities in the uppermost inner core has been described at th...
[1] Mining of the database produced by seismic array stations of the International Monitoring System...
Significant lateral and depth variations of the inner core's properties, such as the large-scale hem...
International audienceConstraining the topography of the inner core boundary (ICB) is important for ...
We investigate arrivals of seismic phases reflected from the core-mantle boundary (PcP waves) and th...
Abstract. We analyze reflections from the Earth’s inner core boundary (ICB) and coda waves following...
Frequency-dependent reflection coefficients of P waves at the inner core boundary (ICB) are estimate...
Abstract We assembled a database consisting of 5,404 PKIKP/PKiKP observations from 555 events, where...
International audienceConstraining the topography of the ICB is important for studies of core-mantle...
The inner core boundary marks the phase transition between the solid inner core and the fluid outer ...
The structure of the Earth's inner core is not well known between depths of ∼100–200 km beneath the ...
The idea of Earth inner core anisotropy is well-established, and it is a very important topic in und...
Travel times, listed in the I.S.S., of longitudinal waves at distances of 100 " < A < 115...
The structure of the Earth’s inner core is not well known between depths of ∼100–200 km beneath the ...
The seismic phase PKiKP, reflected from the inner core, and its coda give information on the short s...
The hemispherical pattern of seismic velocities in the uppermost inner core has been described at th...
[1] Mining of the database produced by seismic array stations of the International Monitoring System...
Significant lateral and depth variations of the inner core's properties, such as the large-scale hem...
International audienceConstraining the topography of the inner core boundary (ICB) is important for ...
We investigate arrivals of seismic phases reflected from the core-mantle boundary (PcP waves) and th...
Abstract. We analyze reflections from the Earth’s inner core boundary (ICB) and coda waves following...
Frequency-dependent reflection coefficients of P waves at the inner core boundary (ICB) are estimate...
Abstract We assembled a database consisting of 5,404 PKIKP/PKiKP observations from 555 events, where...
International audienceConstraining the topography of the ICB is important for studies of core-mantle...
The inner core boundary marks the phase transition between the solid inner core and the fluid outer ...
The structure of the Earth's inner core is not well known between depths of ∼100–200 km beneath the ...
The idea of Earth inner core anisotropy is well-established, and it is a very important topic in und...
Travel times, listed in the I.S.S., of longitudinal waves at distances of 100 " < A < 115...
The structure of the Earth’s inner core is not well known between depths of ∼100–200 km beneath the ...