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REVIEW 4 major objections 5 minor 1 cited by

Towards End-to-End Earthquake Monitoring Using a Multitask Deep Learning Model

T0 review · 4 major / 5 minor · reviewed 2026-08-07 · deepseek-v4-flash

Pith's one-line read PhaseNet+ simultaneously picks phases, reads polarities, and estimates origin times from raw waveforms.

desk verdict Useful incremental multitask model with a genuinely new combination, but the origin-time association claim is under-specified and not independently validated. read the letter →

arxiv 2506.06939 v1 pith:UKDXFZYM submitted 2025-06-07 physics.geo-ph

classification physics.geo-ph
keywords multitaskdeeplearningseismicphasepickingfirst-motionpolarityassociationorigintimepredictionRidgecrestearthquakesequencefocalmechanismsNet+
verification ladder T0 review T1 audit T2 compute T3 formal

The pith

A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.

The reading

This paper claims that one deep network can replace the usual chain of separate seismology tools by simultaneously picking P and S arrival times, reading first-motion polarity, and predicting event origin times directly from continuous waveforms. The authors extend PhaseNet, a U-Net phase picker, into PhaseNet+ by adding two branches: one that classifies polarity on the vertical component and one that detects events and regresses origin time. The origin-time prediction is meant to simplify phase association: instead of searching over travel-time moveouts, the network groups picks that share a common origin time. If this works, a single forward pass over a waveform archive yields the measurements needed to build earthquake catalogs with locations and focal mechanisms, avoiding information loss and repeated scanning. The paper reports that on the 2019 Ridgecrest sequence the approach rivals dedicated association methods and yields up to 7,815 focal mechanism solutions versus 1,875 in the routine catalog.

What carries the argument

The central object is the multitask U-Net architecture of PhaseNet+: a shared encoder feeding three branches, namely a phase arrival-time segmentation branch that labels P, S, and noise; a polarity branch that outputs a per-sample score in $[-1,1]$ on the vertical component; and an event-detection branch that both segments the midpoint of P and S arrival times and regresses the origin time. The load-bearing identity is the station-level origin-time proxy: the midpoint of P and S arrival times approximates the origin time up to a distance-dependent offset, and the regression branch learns that correction, so phase association reduces to grouping picks with similar predicted origin times. This shared-encoder design lets the three tasks reinforce one another, and the origin-time branch is what makes a single forward pass sufficient to provide association constraints.

What would settle it

Apply PhaseNet+ to a sequence with a high-precision reference catalog that includes near-simultaneous earthquakes, and check whether predicted origin times separate events whose true origin times differ by less than about 2 s; if a substantial fraction of associations merge or split at that threshold, the origin-time short-cut fails. A companion check is to measure origin-time prediction error as a function of epicentral distance beyond about 100 km, since the paper already reports growing errors for travel times exceeding 15 s, and to test whether association accuracy degrades exactly in that regime.

Watch

Extended reading notes

Core claim

PhaseNet+ performs phase arrival-time picking, first-motion polarity determination, and origin-time prediction for phase association in a single forward pass, built on a shared U-Net encoder with three output branches. The phase arrival and polarity branches share hidden layers; polarity is scored in $[-1,1]$ at every sample of the vertical component, and the arrival-time branch determines where on the waveform the polarity score is read. Event detection is framed as a segmentation task that locates the midpoint of P and S arrival times, and the origin time is predicted by regression, so that phase association becomes the grouping of picks with similar predicted origin times. Trained on the California Earthquake Event Dataset, the model matches PhaseNet in pick timing, matches or beats the CNN Ross baseline in polarity classification, and keeps origin-time errors mostly within 2 s. In the 2019 Ridgecrest application, the workflow produced 23,103 events (73-81% more than the SCSN catalog), less spatial scatter than the GaMMA-based reference association, and up to 7,815 focal mechanism solutions from combined polarity and S/P amplitude ratio data.

Load-bearing premise

The load-bearing premise is that a station-level origin-time estimate, learned from the average of P and S arrival times with errors mostly within 2 s, is accurate enough to separate distinct earthquakes even in dense aftershock sequences where events can occur nearly simultaneously.

Editorial extensions

If this is right

  • A single scan of continuous waveforms can yield picks, polarities, and origin times, so earthquake catalogs can be built without running separate phase-picking, polarity-picking, and association models.
  • Because polarity is extracted directly from the phase-arrival branch, the model reclassifies roughly 50-60% of manual 'unknown' polarities as up or down, increasing the yield of usable first-motion readings for focal mechanism inversions.
  • On the 2019 Ridgecrest sequence the end-to-end workflow produced 73-81% more events than the SCSN catalog and focal mechanism counts up to about four times SCSN's, with faulting style and stress directions consistent across catalogs.
  • The multitask template is not specific to PhaseNet: any sequence-to-sequence phase picker, such as EQTransformer or PhaseNO, can be extended the same way.
  • The workflow separates perception (picking, polarity, association constraints) from physics-based inversion (location, focal mechanism), so deep learning handles pattern recognition while geophysical inversion preserves physical constraints.

Reading between the lines

Editorial extensions of the paper, not claims the author makes directly.

  • If the origin-time proxy degrades with distance, as the paper's own error growth beyond 15 s travel time suggests, the association shortcut may need a distance-aware correction or a hybrid approach when networks include far stations.
  • The multitask design could be extended to multi-station input, so that origin-time consistency across stations is learned jointly rather than combined afterwards; the paper notes this as a possibility but does not implement it.
  • Applying PhaseNet+ to induced or volcanic sequences, where event rates and waveform similarity differ from California, would test whether the polarity-reclassification gain and origin-time association margins transfer beyond the training region.
  • The reported four-fold increase in focal mechanisms implies that even small events, which routine catalogs leave without mechanisms, may carry usable polarity information; this could change how completeness of mechanism catalogs is measured.
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Editorial analysis

A structured set of objections, weighed in public.

Desk editor's note, referee report, and a circularity audit.

Referee Report

4 major / 5 minor

Summary. The manuscript presents PhaseNet+, a multitask extension of the PhaseNet phase-picking architecture that jointly outputs P/S arrival-time picks, first-motion polarities, and a per-station origin-time estimate intended to support phase association. The authors train PhaseNet+ on the Northern California portion of the CEED dataset and evaluate it on 2023 data from Northern and Southern California, comparing phase picking with PhaseNet, polarity picking with the CNN Ross model, and origin-time accuracy against manually reviewed labels. They then apply the model to one week of the 2019 Ridgecrest sequence, producing an event catalog via origin-time-based association and a focal-mechanism catalog using SKHASH. The reported results show phase-picking parity with PhaseNet, polarity accuracy comparable or superior to the CNN Ross baseline, origin-time errors mostly within 2 s, a PhaseNet+ catalog with 73–81% more events than SCSN and less spatial scatter than a GaMMA catalog built from the same picks, and up to 7,815 focal mechanism solutions. The central claim is that origin-time prediction enables a simplified end-to-end association workflow that rivals dedicated phase association methods.

Significance. If the central claim is upheld, PhaseNet+ would be a practically valuable contribution: a single model that simultaneously provides phase picks, polarities, and origin-time constraints could streamline earthquake monitoring pipelines and make focal-mechanism catalogs much more complete. The authors provide code and promise SeisBench integration, and the training/evaluation on a large, publicly available dataset is a strength. The phase-picking comparison against PhaseNet is a clean same-training-set test, and the Ridgecrest application demonstrates a realistic use case. However, the novelty rests on the origin-time association concept, and that concept is underspecified and under-validated in the manuscript as written. Because the association step is not described as an algorithm and is only tested on preselected single-event waveforms, the event-catalog comparisons in Section 3.2 are not yet sufficient to establish that PhaseNet+ rivals state-of-the-art association methods.

major comments (4)
  1. [§2.1, phase association paragraph] The manuscript says phase association 'simplifies to identifying picks with shared onset times,' but no concrete algorithm is given. There is no description of how per-station origin-time predictions are turned into associated events: no clustering method, no threshold on origin-time agreement, no procedure for handling multiple events at one station, and no treatment of false or missing origin-time predictions. This is the core novelty of the paper, and without this specification the PhaseNet+ catalog in §3.2 cannot be reproduced and the comparison with GaMMA is not interpretable. The authors should provide a precise association procedure, including any hyperparameters, or clearly state that the association is performed by an external algorithm whose inputs include the origin-time predictions.
  2. [§3.2 and Figure 9] The claim that the end-to-end approach 'rival[s] state-of-the-art methods' is supported only by internal comparisons: the PhaseNet+ catalog is compared with SCSN and with a GaMMA catalog built from the same PhaseNet+ picks, but there is no independent ground-truth association reference. The 73–81% increase in event count over SCSN and the reduced spatial scatter relative to GaMMA could be influenced by association artifacts, such as splitting one earthquake into multiple events or merging distinct events with similar origin times. The acknowledged limitation in §4 that origin-time association 'becomes less effective when multiple earthquakes occur nearly simultaneously' is directly relevant to the dense aftershock setting of the Ridgecrest application. A validation against a high-quality reference catalog for the same period, e.g., Shelly (2020), or against at least a set of manually reviewed associations, is needed before the 'rival state-of-the-art' conclusion can be accepted.
  3. [§3.1.2 and Figure 5] The polarity comparison with 'CNN Ross' is not apples-to-apples. The CNN Ross model is described as pre-trained on Southern California data prior to 2018, whereas PhaseNet+ was trained on the Northern California CEED training set (with a different task formulation and architecture). On the Southern California 2023 test set, the comparison is between a model trained on Northern California and a model trained on older Southern California data; on the Northern California 2023 test set, CNN Ross is evaluated out-of-region. The conclusion that PhaseNet+ achieves 'comparable or superior performance' is plausible, but the asymmetry in training data makes the quantitative comparison difficult to interpret. The authors should either retrain CNN Ross on the same Northern California training data, or at least clearly qualify the comparison as a benchmark against a published, frozen baseline rather than a matched model comparison.
  4. [§3.1.3 and §4] The origin-time accuracy evaluation in Figure 7 is performed on isolated, pre-selected test waveforms, not on continuous data with overlapping or near-simultaneous events. The stated purpose of origin-time prediction is phase association in continuous data, yet no experiment measures how well the origin-time predictions separate distinct events in a continuous stream. The §4 statement that the approach 'becomes less effective when multiple earthquakes occur nearly simultaneously, e.g., in dense aftershock sequences' is in tension with the §3.2 claim that the method 'works as effectively for dense aftershocks as dedicated phase association algorithms.' The authors should add a continuous-data evaluation, even a small annotated segment, that tests association performance against known event times, or explicitly narrow the claim about dense aftershock performance.
minor comments (5)
  1. [§3.2, paragraph on catalogs] The SCSN earthquake catalog is attributed to Yang et al. (2012), but Yang et al. (2012) is the Southern California focal mechanism catalog; the routine SCSN event catalog is more commonly attributed to the Southern California Seismic Network/SCEDC (e.g., Hutton et al., 2010). Please clarify the source of the SCSN event catalog used in Figure 9.
  2. [Open research statement] The code is hosted in the EQNet repository, but the paper announces PhaseNet+ as an extension; please provide a specific tag, branch, or model checkpoint identifier so that the exact PhaseNet+ version trained and evaluated here can be retrieved reproducibly.
  3. [Figure 8 caption] The caption says 'green ticks indicating predicted earthquake origin times' but the histogram in panel (b) is not explicitly linked to the per-station green ticks; a sentence clarifying how the histogram is built from the per-station predictions would improve readability.
  4. [§3.2, focal mechanism section] The inversion with SKHASH uses 'SP amplitude ratio data,' but the manuscript does not describe how the S/P amplitude ratios are measured from the PhaseNet+ outputs or whether they come from a separate routine. A brief description or reference for this measurement step would make the focal-mechanism workflow more complete.
  5. [Throughout] There are a few minor grammatical issues, such as 'detecting the average of P and S arrival-times as a segmentation task' in §2.1, where 'detecting' should be 'predicting' or 'estimating' for clarity.

Circularity Check

0 steps flagged · score 0.0 of 10

No significant circularity: the perception tasks are validated on held-out external labels, and the Ridgecrest application is an empirical demonstration rather than a derivation from its own fit.

full rationale

No circularity found. PhaseNet+ is trained on the CEED dataset with manually labeled phase picks, polarities, and origin times, and the task-level evaluations are performed on held-out 2023 Northern and Southern California data against external manual labels, so the per-task performance claims do not reduce to the training labels. The Ridgecrest application is an empirical case study: model outputs are processed by ADLoc and SKHASH and compared with SCSN, a GaMMA catalog built from the same picks, and the Cheng et al. (2023) catalog. The GaMMA reference and PhaseNet+ sharing the same PhaseNet+ picks means the comparison isolates the association mechanism, but this is a validation-design limitation, not a circular derivation. The origin-time association step is not fully specified (no clustering algorithm, threshold, or handling of overlapping events is given), which is a reproducibility concern, not a self-referential reduction. The paper's own Section 4 explicitly acknowledges that origin-time association 'becomes less effective when multiple earthquakes occur nearly simultaneously, e.g., in dense aftershock sequences,' further showing that the limitation is disclosed rather than hidden. Citations to the authors' prior PhaseNet, CEED, GaMMA, EQNet, and ADLoc work are normal method-building and baseline references; they are independent published tools and do not import the present paper's results as premises. No equation, fitted parameter, or learned target is renamed as a prediction in a way that forces the central claims.

Assumptions & free parameters 2 free parameters · 3 assumptions · 0 invented entities

The central claim depends on the origin-time proxy, the trustworthiness of the training labels, and the shared-representation assumption. No new physical entities are introduced. Free parameters are limited to hand-chosen polarity thresholds and the polarity loss weight; other hyperparameters are standard training choices.

free parameters (2)
  • Polarity score thresholds = +/-0.33
    Hand-chosen thresholds map continuous polarity scores to D/N/U labels and are used in all polarity comparisons in section 3.1.2.
  • Polarity loss weight = 0.2
    Chosen to balance multitask losses so they converge to similar scales, as stated in the Discussion (section 4).
assumptions (3)
  • domain assumption A station-level origin time can be approximated by the average of P and S arrival times.
    The event detection branch is trained to detect the average of P and S arrival-times as a proxy for origin time (section 2.1). The approximation is distance dependent and the paper accepts 'occasional ambiguities' for events with similar midpoints.
  • domain assumption Manual phase picks and polarity labels in the CEED and NCEDC/SCEDC datasets are accurate enough to serve as ground truth.
    Training and evaluation use these labels without independent verification, and section 3.1.2 acknowledges that many manual polarity labels are ambiguous, with the model sometimes providing more reasonable predictions.
  • domain assumption A shared U-Net-style encoder can learn representations useful for all three tasks simultaneously.
    The multitask premise (sections 1 and 2.1) assumes mutual information among picking, polarity, and origin time can be exploited by one hidden representation. No independent evidence is provided beyond the reported results.

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Cite this review

Pith. "Pith review of Towards End-to-End Earthquake Monitoring Using a Multitask Deep Learning Model." pith.science (2026). https://pith.science/paper/UKDXFZYM

@misc{pith2026250606939,
  author       = {Pith},
  title        = {Pith review of: Towards End-to-End Earthquake Monitoring Using a Multitask Deep Learning Model},
  year         = {2026},
  howpublished = {\url{https://pith.science/paper/UKDXFZYM}},
  note         = {Machine review of arXiv:2506.06939}
}
read the original abstract

Seismic waveforms contain rich information about earthquake processes, making effective data analysis crucial for earthquake monitoring, source characterization, and seismic hazard assessment. With rapid developments in deep learning, the state-of-the-art approach in artificial intelligence, many neural network models have been developed to enhance earthquake monitoring tasks, such as earthquake detection, phase picking, and phase association. However, most current efforts focus on developing separate models for each specific task, leaving the potential of an end-to-end framework relatively unexplored. To address this gap, we extend an existing phase picking model, PhaseNet, to create a multitask framework. This extended model, PhaseNet+, simultaneously performs phase arrival-time picking, first-motion polarity determination, and phase association. The outputs from these perception-based models can then be processed by specialized physics-based algorithms to accurately determine earthquake location and focal mechanism. The multitask approach is not limited to the PhaseNet model and can be applied to other state-of-the-art phase picking models, ultimately improving seismic monitoring through a more unified and efficient approach.

Figures

Figures reproduced from arXiv: 2506.06939 by the authors.

Figure 1
Figure 1. Neural network architecture of the PhaseNet+ designed for simultaneous phase arrival-time picking, [PITH_FULL_IMAGE:figures/full_fig_p006_1.png] view at source ↗
Figure 2
Figure 2. Example of PhaseNet+ predictions demonstrating the model’s multitask capabilities. The model [PITH_FULL_IMAGE:figures/full_fig_p006_2.png] view at source ↗
Figure 3
Figure 3. Overview of the end-to-end approach to earthquake monitoring based on a multi-task model. The [PITH_FULL_IMAGE:figures/full_fig_p007_3.png] view at source ↗
Figures from the paper (9 more)
Figure 4
Figure 4. Figure 4: Comparison of phase arrival-time picking performance between PhaseNet+ and PhaseNet models [PITH_FULL_IMAGE:figures/full_fig_p008_4.png]
Figure 5
Figure 5. Figure 5: Comparison of polarity picking performance between PhaseNet+ and the CNN [PITH_FULL_IMAGE:figures/full_fig_p009_5.png]
Figure 6
Figure 6. Figure 6: Examples of mismatched polarities between manual labels and PhaseNet+ model predictions: [PITH_FULL_IMAGE:figures/full_fig_p010_6.png]
Figure 7
Figure 7. Figure 7: Origin time prediction performance of PhaseNet+ evaluated on (a) Northern and (b) Southern [PITH_FULL_IMAGE:figures/full_fig_p011_7.png]
Figure 8
Figure 8. Figure 8: Example of PhaseNet+ predictions for an event from the Ridgecrest sequence (event ID: [PITH_FULL_IMAGE:figures/full_fig_p013_8.png]
Figure 9
Figure 9. Figure 9: Comparison of (a) temporal distribution of event frequency, (b) magnitude distribution, and (c) [PITH_FULL_IMAGE:figures/full_fig_p014_9.png]
Figure 10
Figure 10. Figure 10: Spatial distribution of earthquakes from (a) SCSN catalog, (b) GaMMA catalog, and (c) [PITH_FULL_IMAGE:figures/full_fig_p015_10.png]
Figure 11
Figure 11. Figure 11: Spatial distribution of P-axis azimuths from focal mechanism solutions: (a) SCSN catalog, (b) [PITH_FULL_IMAGE:figures/full_fig_p016_11.png]
Figure 12
Figure 12. Figure 12: Spatial distribution of scalar faulting types derived from focal mechanism solutions: (a) SCSN [PITH_FULL_IMAGE:figures/full_fig_p017_12.png]

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Forward citations

Cited by 1 Pith paper

Reviewed papers in the Pith corpus that reference this work. Sorted by Pith novelty score. Full citation record

  1. VORA: Rapid Association of Earthquake Phases from Local to Global

    physics.geo-ph 2026-07 conditional novelty 6.0 of 10

    VORA associates earthquake phases via unsupervised spatio-temporal clustering of origin times on a Voronoi station graph, delivering fastest runtime and local-to-global scalability without training.

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Reviewed August 7, 2026 · model on record in the stance chip above.