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Record W4411141344 · doi:10.1130/b37994.1

Dextral slip along the Western Nepal Fault System accommodates significant orogen-parallel shear

2025· article· en· W4411141344 on OpenAlexaff
Andrew K.R. Hoxey, Michael H. Taylor, Michael A. Murphy, Sean P. Bemis, Deepak Chamlagain, Richard Styron, Elaina J. Sutley, Basanta Raj Adhikari, Suoya Fan, M. K. Daniel, Elizabeth Curtiss, Manoj Kafle, John Gosse, Tammy M. Rittenour

Bibliographic record

VenueGeological Society of America Bulletin · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
Topicearthquake and tectonic studies
Canadian institutionsDalhousie University
Fundersnot available
KeywordsSinistral and dextralGeologySeismologyShear (geology)Strike-slip tectonicsShear zoneNormal faultFault (geology)Slip (aerodynamics)GeodesyPetrologyTectonics

Abstract

fetched live from OpenAlex

Abstract New mapping in northwestern Nepal documents geomorphic landforms that are truncated and offset by active faults along the Western Nepal Fault System (WNFS), a right-slip fault system that accommodates orogen-parallel strain in the West Nepal Himalaya between Simikot and Tansen. Neotectonic field investigations in this study focus on the northwestern segment of the WNFS in the Jumla and Dolpa districts, where field observations of dextral-oblique slip on the Talphi, Kuri Santha, and Tripurakot faults indicate active deformation within the Himalayan thrust wedge. The surface trace of the Talphi fault is expressed by prominent fault scarps, deflected and offset stream channels, and shutter ridges that delineate an ~40 km long, subvertical, ~N40°W striking fault that traverses areas of high topographic relief. Our field mapping documents truncated and offset fluvial terrace risers that, when combined with Quaternary geochronology, suggest a minimum dextral-oblique slip rate of 2.7 ± 0.6 mm/yr since ca. 130 ka. The Kuri Santha fault strikes subparallel to the Talphi fault, and mapping of offset fluvial terrace treads and Quaternary geochronology suggest a minimum fault slip rate of 1.0 ± 0.2 mm/yr since ca. 43 ka. Approximately 60 km to the southeast, near Tripurakot, shutter ridges provide compelling evidence for dextral displacement along an ~N65°W striking, steeply northeast dipping fault. Several geomorphic features documented along strike of the Talphi, Kuri Santha, and Tripurakot faults are consistent with surface expressions of active structures, suggesting all three faults reach >40 km in length. The similar geometry, kinematics, and proximity of the Talphi, Kuri Santha, and Tripurakot faults is consistent with a kinematic link between the structures, which would imply these three surface-rupturing faults could produce large magnitude earthquakes, a critical contribution to seismic hazard and risk analysis in western Nepal. Our data are consistent with a kinematic linkage between the Karakoram fault and a foreland-ward propagation of orogen-parallel strain. The Talphi, Kuri Santha, and Tripurakot faults also show geometric similarities with splay faults in marine subduction zones that accommodate intra-wedge deformation and produce repeated late Quaternary surface ruptures. Our study underscores the importance of understanding intra-wedge fault splays in mega-thrust fault systems, globally.

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)0.000
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 score0.014
Threshold uncertainty score0.027

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0000.000
Scholarly communication0.0010.000
Open science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.015
GPT teacher head0.220
Teacher spread0.205 · 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".

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Citations1
Published2025
Admission routes1
Has abstractyes

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