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Inferring Earth’s discontinuous chemical layering from the 660-kilometer boundary topography
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Journal Article
Inferring Earth’s discontinuous chemical layering from the 660-kilometer boundary topography
2019
Overview
Topography, or depth variation, of certain interfaces in the solid Earth can provide important insights into the dynamics of our planet interior. Although the intermediate- and long-range topographic variation of the 660-kilometer boundary between Earth’s upper and lower mantle is well studied, small-scale measurements are far more challenging. We found a surprising amount of topography at short length scale along the 660-kilometer boundary in certain regions using scattered P′P′ seismic waves. Our observations required chemical layering in regions with high short-scale roughness. By contrast, we did not see such small-scale topography along the 410-kilometer boundary in the upper mantle. Our findings support the concept of partially blocked or imperfect circulation between the upper and lower mantle.
Publisher
American Association for the Advancement of Science,The American Association for the Advancement of Science
Subject
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