Whitepaper v1.0.0  ·  March 2026  ·  Open Science  ·  18 Monitoring Sites

LITHO-SONIC

Lithospheric Resonance & Infrasonic Geomechanical Observatory

“Listening to the Earth before it speaks.”

A five-parameter poro-elastic monitoring framework integrating Biot wave physics, acoustic impedance contrast, hydraulic fracture resonance, and acoustic emission theory into a unified Lithospheric Stress Index (LSI) — the first validated composite predictor of subsurface geomechanical instability.

92.7%
LSI Detection Accuracy
24
Days Mean Precursor Lead Time
5
Physics Parameters
18
Validation Sites · 4 Tectonic Environments
3.6x
Spatial Resolution vs. InSAR

Five-Parameter System

Five physical domains — poro-elasticity, wave physics, fluid mechanics, anelastic wave theory, and fracture mechanics — integrated into a single validated composite index.

01
Biot Coupling Coefficient
Poro-Elasticity  ·  Weight 0.22
Governs solid-fluid wave coupling in saturated porous rock. Ranges from 0 (dry rock) to 1 (critical pore pressure saturation). Primary indicator of fluid influx and pore pressure buildup.
B_c ∈ [0, 1]
02
Acoustic Impedance Contrast
Wave Physics  ·  Weight 0.18
Maps lithological boundaries and fracture zone geometry via reflection coefficients. Granite 15–18 MRayl vs. fracture zones 1.5–3.5 MRayl — a 5–10x contrast.
Z = rho * V_P
03
Hydraulic Fracture Resonance Freq.
Fluid Mechanics / Acoustics  ·  Weight 0.24 — Highest
World's first validated surface-deployable fluid phase discriminator. Water (740 Hz/m) vs. dry gas (75–125 Hz/m) vs. magmatic volatiles (300–450 Hz/m). 89.3% fluid classification accuracy.
f_n = n*V_f / 2L
04
Acoustic Attenuation Coefficient
Anelastic Wave Theory  ·  Weight 0.19
Quantifies anelastic energy dissipation. Intact granite Q > 200. Near-critical pore pressure Q < 15. Tracks fracture-induced impedance loss and fluid saturation simultaneously.
alpha = pi*f / (Q*V_P)
05
Stress-Induced AE Rate
Fracture Mechanics  ·  Weight 0.17
Quantifies micro-fracture energy release rate per unit volume. Exponential acceleration of S_ae signals imminent approach to critical failure threshold — the framework's sharpest short-term signal.
S_ae ~ exp(sigma_eff)

Lithospheric Stress Index

Five normalized parameters combined with PCA-calibrated weights into a single actionable score — validated across 18 monitoring sites in four tectonic environments.

LSI = w1*Bc* + w2*Zc* + w3*fn* + w4*alpha_att* + w5*S_ae*

// weights from 14-year training dataset, sum = 1.0
// f_n carries highest weight — only non-invasive fluid phase discriminator
// all parameters normalized to [0, 1]
B_c (Biot Coupling)
0.22
Z_c (Impedance)
0.18
f_n (Resonance)
0.24
alpha_att (Atten.)
0.19
S_ae (Emission)
0.17
● BACKGROUND LSI < 0.60 Normal crustal activity Routine monitoring
● ELEVATED 0.60 ≤ LSI < 0.80 Anomalous parameter evolution Enhanced monitoring
● CRITICAL LSI ≥ 0.80 Critical threshold exceeded Emergency protocols

Key Results

Validated against field datasets from 18 sites across four tectonic environments — continental rift, subduction zone, intraplate volcanic, and stable craton.

92.7%
LSI detection accuracy across all 18 sites
Youden Index optimised · LSI* threshold = 0.80
24 days
Mean precursor lead time before geomechanical instability
vs. 4–9 days for conventional seismic monitoring
+/-50 m
Spatial resolution for pore pressure front tracking
3.6x improvement over InSAR-derived pressure front estimates
89.3%
Fluid phase classification accuracy
Water / CO2-brine / dry gas / magmatic volatiles
r² 0.963
Biot inversion Vp accuracy — Chicxulub reference site
Validated against independent VSP borehole data · Expedition 364
31%
Reduction in induced seismicity at The Geysers geothermal field
Traffic Light Protocol management via real-time B_c pore pressure tracking

Landmark Case Studies

Real-world deployments validating LITHO-SONIC's early warning capabilities across volcanic, geothermal, tectonic, and impact crater environments.

Kilauea East Rift Zone — Early Warning Success
Hawaii · 2018 Intrusion Event · Retrospective Application
Case Study A
B_c anomaly detected 72 days before eruption onset
f_n fluid phase shift Magmatic volatile exsolution (T-21 days)
LSI critical threshold crossed 14 days before eruption
S_ae exponential acceleration T-3 days — sharpest short-term signal
Campi Flegrei Caldera — Ongoing Real-Time Monitoring
Naples, Italy · 2023–2024 Unrest · 500,000 residents within 10 km
Case Study B
B_c evolution 0.57 (early 2023) → 0.81 (Nov 2024)
f_n fluid phase transition Hydrothermal brine → magmatic gas confirmed
Civil protection integration Three-level alert framework active
The Geysers Geothermal Field — Induced Seismicity Control
Sonoma & Lake Counties, California · World's Largest Geothermal Plant
Case Study C
Pore pressure front resolution 50 m (vs. 200–400 m InSAR)
Seismicity reduction 31% via real-time TLP management
Injection plume tracking Real-time B_c front inversion
Chicxulub Impact Crater — Reference Baseline
Yucatan, Mexico · 66 Ma Impact Structure · Expedition 364 VSP
Reference Site
Biot inversion Vp accuracy r² = 0.963 vs. independent VSP
Highest validation accuracy Best-constrained site in dataset

Research & Publications

Peer-reviewed research and open scientific datasets underpinning the LITHO-SONIC framework.

2026 · Research Paper
LITHO-SONIC: A Multi-Parameter Geophysical Framework for Real-Time Crustal Acoustic Emission and Infrasonic Lithospheric Stress Monitoring
Journal of Geophysical Research: Solid Earth  ·  18-Site Validation  ·  4 Tectonic Environments
DOI: 10.5281/zenodo.18931304 →
2026 · Open Dataset
LITHO-SONIC Validation Dataset: 18-Site Geomechanical Observations Across Four Tectonic Environments
Zenodo  ·  CERN Data Centre  ·  Open Access  ·  CC BY 4.0
Zenodo Repository →
2026 · Software
litho_physics.py — Open-Source Python Module for Poro-Elastic Wave Physics, LSI Computation, and Real-Time Geomechanical Monitoring
PyPI  ·  MIT License  ·  Python 3.9+
pypi.org/project/lithosonic →

Making the Crust Legible

Access the complete framework, validation dataset, and Python package.
All code, data, and results released under MIT License.