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06RESEARCH PAPERPreprint

From Waveform Inversion to Deep-Earth Anomalies: A Formal Working Paper on Membranous High-Pressure Structures, Observational Limits, and the Epistemic Status of Speculative Geophysical Models

Chen, Ho Yiing

發表日期

DOI 10.5281/zenodo.21257561 Zenodo 紀錄頁 PDF(113 KB)

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摘要

ABSTRACTZenodo 原文
This paper formalizes a speculative but non-arbitrary line of reasoning concerning the epistemic limits of human knowledge about the deep Earth. The central claim is not that a literal hollow Earth or inhabitable underground world exists. Rather, the paper asks whether complex, high-pressure, multi-layered, shell-like or membrane-like anomalous regions could be under-resolved or over-smoothed by present geophysical inverse models. The argument begins from an observation: human knowledge of the mantle, core-mantle boundary, outer core, and inner core is overwhelmingly indirect, mediated by seismic waves, gravity fields, magnetic fields, normal modes, heat-flow constraints, mineral physics, and model-based inversion. This makes planetary interior science powerful but not equivalent to direct inspection. We introduce the Membranous Deep-Earth Anomaly Hypothesis (MDEAH): under billions of years of high pressure, high temperature, convection, phase transitions, slab subduction, partial melting, chemical segregation, and core-mantle coupling, the interior may contain multi-scale, layered, shell-like, high-pressure anomalies whose true geometry may be more complex than current smoothed velocity or density models suggest. The hypothesis is distinguished from a literal hollow-Earth claim. It is framed as a testable residual hypothesis: if such structures exist, they should appear as systematic residuals in seismic travel times, waveform scattering, normal-mode splitting, gravity-density inversions, geomagnetic coupling, and eventually neutrino tomography. Mathematically, the paper uses the language of forward modeling and inverse problems, showing that geophysical observations satisfy equations of the form d=F(m)+\epsilon, where m is an internal Earth model, F is a forward operator, and \epsilon is noise and modeling error. Because F^{-1} is generally non-unique and resolution-limited, the absence of a feature in a model is not equivalent to a proof that no such structure exists. At the same time, large low-density voids are strongly constrained by mass, moment of inertia, seismic-wave propagation, and pressure stability. Thus, the scientifically defensible version of the speculation is not an empty cavity, but a high-P anomalous domain: a complex, possibly shell-like, partially molten, dense, low-velocity, anisotropic, or otherwise exotic region that may be simplified by current inversions. The conclusion is deliberately balanced. Present evidence strongly disfavors literal large empty caverns below it, but it does not eliminate the possibility that deep-Earth anomalies are structurally richer than current models can resolve. The value of the hypothesis lies not in claiming discovery, but in converting intuition into falsifiable questions, residual tests, and multi-observable predictions. Copyright (c) 2026 Chen, Ho Yiing (norika). Licensed under Creative Commons Attribution 4.0 International (CC BY 4.0).
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全文 PDF

FULL TEXT1 個檔
  • 下載 PDFwave_inversion_deep_earth_paper.pdf・113 KB・本站

PDF 與 Zenodo 上的檔案相同(大小與 md5 已核對)。

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論文資料

DETAILSZenodo 紀錄 21257561
作者
Chen, Ho Yiing
發表日期
資源類型
Preprint
DOI
10.5281/zenodo.21257561
Zenodo
zenodo.org/records/21257561
授權
Creative Commons Attribution 4.0 International

作者 Chen, Ho Yiing 是織田紀香的本名(陳禾穎)英文拼寫。標題、摘要、關鍵字與授權照 Zenodo 原文。

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關鍵字

KEYWORDS20 個
  • waveform inversion
  • deep-Earth anomalies
  • inverse problem
  • seismic tomography
  • LLSVP
  • ULVZ
  • MDEAH
  • membranous anomaly hypothesis
  • high-pressure structures
  • core-mantle boundary
  • model resolution
  • non-uniqueness
  • epistemic limits of geophysics
  • residual analysis
  • normal-mode splitting
  • gravity-density inconsistency
  • neutrino tomography
  • ER=EPR analogy
  • emergent spacetime
  • wave-form ontology
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