Morphology and possible origins of the Perm anomaly in the lowermost mantle of Earth

IF 2.9 3区 地球科学
YuMei He, LianXing Wen, Yann Capdeville
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Abstract

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 small-scale chemical pile in the lowermost mantle, although the hypothesis of a developing mantle plume cannot be ruled out.

Abstract Image

地球最下层地幔中Perm异常的形态和可能的起源
利用走时分析和地幔地震数据采样的三维正演波形建模,我们在地幔下的核心-地幔边界(即Perm异常)附近约束了一个小型的、圆顶状的低速结构。最合适的圆顶模型以东经60.0°,北纬50.5°为中心,高度为400公里,半径从顶部的200公里增加到CMB的450公里。它的速度减少从顶部的0%到CMB上方240公里处的-3.0%到CMB处的-3.5%不等。在其周围还发现了一个240公里厚的高速D”结构。虽然不能排除地幔柱发育的假说,但Perm异常可能代表了最下层地幔中一个稳定的小规模化学堆。
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来源期刊
Earth and Planetary Physics
Earth and Planetary Physics GEOSCIENCES, MULTIDISCIPLINARY-
自引率
17.20%
发文量
174
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