作者:YuMei He,LianXing Wen,Yann Capdeville
摘要:We have constrained a small-scale,dome-shaped low-velocity structure near the core-mantle boundary(CMB)of Earth beneath Perm(the Perm anomaly)using travel-time analysis and three-dimensional(3-D)forward waveform modeling of seismic data sampling of the mantle.The best-fitting dome-shaped model centers at 60.0°E,50.5°N,and has a height of 400 km and a radius that increases from 200 km at the top to 450 km at the CMB.Its velocity reduction varies from 0%at the top to–3.0%at 240km above the CMB to–3.5%at the CMB.A surrounding 240-km-thick high-velocity D''structure has also been detected.The Perm anomaly may represent a stable smallscale chemical pile in the lowermost mantle,although the hypothesis of a developing mantle plume cannot be ruled out.
发文机构:Key Laboratory of Earth and Planetary Physics Mohe Observatory of Geophysics Laboratory of Seismology and Physics of Earth’s Interior Department of Geosciences Laboratoire de Planétologie et Géodynamique de Nantes
关键词:seismicvelocitystructurecore-mantleboundaryPermanomalychemicalpile
分类号: P31[天文地球—固体地球物理学]