On the origin of mid-mantle discontinuities beneath the Central Pacific as revealed by long-period SS and PP precursors
Carr, Steve A.B., Olugboji, Tolulope, Waszek, Lauren, Zhang, Ziqi, and Schmerr, Nicholas C. (2026) On the origin of mid-mantle discontinuities beneath the Central Pacific as revealed by long-period SS and PP precursors. Geophysical Journal International, 246 (3). ggag266.
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Abstract
The origin of seismic discontinuities in the Earth’s mid-mantle ((Formula presented) 700–1400 km) remains debated, with competing hypotheses attributing them to either partial melting due to water transport across the transition zone or compositional heterogeneities (subducted crust). Distinguishing between these scenarios has been hindered by the inability of standard imaging techniques to extract robustly the polarity of weak seismic reflections amidst noise and reverberations that contaminate mid-mantle reflections. Here, we introduce a novel signal processing framework that combines curvelet-based wavefield separation with extended multitaper deconvolution to resolve this polarity ambiguity. We validate this approach by applying it to a high-quality data set of SS and PP precursors beneath the Central Pacific. This application yields the robust detection of a discontinuity at approximately 800 km depth, characterized by a sharp positive shear velocity contrast ((Formula presented)) and a negligible density contrast. The observed positive polarity precludes partial melt or thermal plumes as primary causal mechanisms. Instead, the high-velocity, neutral-density signature is consistent with a layer of stagnant, subducted oceanic crust in thermal equilibration with the ambient mantle. These results demonstrate the efficacy of the deconvolution framework and provide direct seismic evidence for compositional stratification in the mid-mantle, supporting geodynamic models where viscosity increases facilitate the long-term preservation of recycled lithosphere. © The Author(s) 2026. Published by Oxford University Press on behalf of The Royal Astronomical Society. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited.
| Item ID: | 92683 |
|---|---|
| Item Type: | Article (Research - C1) |
| ISSN: | 1365-246X |
| Copyright Information: | © The Author(s) 2026. Published by Oxford University Press on behalf of The Royal Astronomical Society. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited. |
| Date Deposited: | 10 Aug 2026 05:47 |
| FoR Codes: | 37 EARTH SCIENCES > 3706 Geophysics > 370609 Seismology and seismic exploration @ 100% |
| SEO Codes: | 28 EXPANDING KNOWLEDGE > 2801 Expanding knowledge > 280107 Expanding knowledge in the earth sciences @ 100% |
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