MétaCan
Menu
Back to cohort
Record W7135701194

Which operational factors lead to seismogenic fluid-injections? observations from ten large-scale studies in North America

2025· article· en· W7135701194 on OpenAlexaboutno aff
Iason Grigoratos, Alexandros Savvaidis, German Rodriguez, James P. Verdon, S. Wiemer

Bibliographic record

VenueBristol Research (University of Bristol) · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
Topicearthquake and tectonic studies
Canadian institutionsnot available
FundersU.S. Geological Survey
KeywordsInduced seismicityTectonicsLead (geology)Block (permutation group theory)Sedimentary rockHydraulic fracturingSeismic energy
DOInot available

Abstract

fetched live from OpenAlex

We investigated for the first time the role wastewater disposal (SWD) and hydraulic fracturing (HF) played throughout North America, under the same statistical framework. We employed new earthquake catalogs, novel declustering techniques and established physics-based principles. Our datasets included 600’000 SWD wells, 219’000 HF stimulations and 93’000 earthquakes from Oklahoma, Kansas, Western Canada Sedimentary Basin, Delaware basin, Eagle Ford play, Midland basin, Fort Worth Basin, Raton basin, Arkansas. Following Grigoratos et al. (2020. 2022), we first hindcasted the seismicity rates on a spatial grid using either actual or randomized injection data as input. In the end, each block is confidence level for its causal link with either HF or SWD. We classified each event as tectonic or triggered by SWD or HF, employing the aforementioned confidence intervals, with some additional spatio-temporal well-to-earthquake association filters used for sanity checks. Post-processing the results, we identified which operational factors appear associated with recorded seismicity or elevated magnitudes. Some of our key findings are listed below: HF - a tiny percentage of stimulations is responsible for most of the seismicity - 90% of seismic triggering started during stimulation, thus no need for large time-lags - no correlation between detectable seismic potential and injection rate or total volume - no correlation between seismic potential and stimulation depth, even for larger magnitudes - fault-specific geomechanical conditions dominate across basins; for the EQ rates, the fluid volumes are important only within local sub-km scales SWD - The vast majority of seismogenic wells were <5 km away from the closet earthquake - the injection rate, total volume and distance-to-basement are crucial for seismogenic potential and rupture-size - the absolute well-depth does not affect the magnitude of the triggered seismicity - the Mmax is not correlated to the Seismogenic Index (Shapiro et al, 2010); thus, reactivating many small faults does not necessarily imply that significantly larger favorable faults are also nearby - the Mmax is much more correlated to the distributed volumes (via pore-pressure diffusion principles) than to “static” injected volumes; thus, the Theis equation is valid for large-scale diffusivity values between 0.3 and 2 m2/s.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.002
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.105
Threshold uncertainty score0.209

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.002
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.002
Science and technology studies0.0000.000
Scholarly communication0.0010.000
Open science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.097
GPT teacher head0.310
Teacher spread0.213 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2025
Admission routes1
Has abstractyes

Explore more

Same venueBristol Research (University of Bristol)Same topicearthquake and tectonic studiesFrench-language works237,207