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Record W4401480531 · doi:10.56952/arma-2024-0358

Exploring Ground Penetrating Radar (GPR) Simulation for Imaging and Determining Electromagnetic Wave Velocity in Volcanogenic Massive Sulfide (VMS) Deposits

2024· article· en· W4401480531 on OpenAlexaff
L. Abbasian, Stephen Butt

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEngineering
TopicGeophysical Methods and Applications
Canadian institutionsMemorial University of Newfoundland
Fundersnot available
KeywordsGround-penetrating radarGeologyRadarElectromagneticsRadar imagingSeismologyRemote sensingGeophysicsAcousticsAerospace engineeringPhysicsEngineeringElectronic engineering

Abstract

fetched live from OpenAlex

ABSTRACT: Ground-Penetrating Radar (GPR) simulation plays a pivotal role in geophysical methods, aiding in survey design, understanding physical behaviour, and quantifying responses. This study employs the gprMax software to simulate the propagation of electromagnetic waves through different Volcanogenic Massive Sulfide (VMS) deposits, each with unique electrical properties. The fundamentals of GPR modeling and factors influencing survey design (operating frequency, recording time window, temporal and spatial sampling interval) are outlined. Careful consideration of these parameters is essential for effective GPR surveys. In addition, results from the simulations of EM wave propagation through VMS minerals such as Galena, Bornite, Magnetite, Pyrite, Sphalerite and Hematite, and their host rocks were utilized to calculate wave velocities in each mineral, rendering it possible to determine the location of Boundaries of VMS veins within the host rock using this method. Some deposits with lower electrical conductivities, showed possibility of being imaged successfully using Electromagnetic (EM) methods. In contrast, some other deposits, having higher electrical conductivities, tended to weaken electromagnetic signals, especially within the frequency range used in GPR applications. This study enhances our comprehension of GPR simulation and its possible uses in geophysics, specifically in the characterization of diverse geophysical materials that possess distinct electrical properties. 1 INTRODUCTION Volcanogenic massive sulfide (VMS) deposits, are key sources of metals like Zn, Cu, Pb, Ag, and Au. Also, there is a substantial proportion of pyrite, or iron sulphide (FeS2) that is frequently connected to VMS occurrences. The economic importance of these deposits is underscored by their contribution to metal production. Most VMS deposits consist of massive (>40 percent) sulphide (typically pyrite, pyrrhotite, chalcopyrite, sphalerite, and galena as well as magnetite) (Best, 2015). These minerals and their associated economic minerals are listed in Table 1. GPR simulation is a powerful tool in delineating VMS deposits, crucial for optimizing GPR survey parameters and understanding mineral-host rock interactions. This approach facilitates accurate mapping and exploration of VMS deposits, enhancing the effectiveness of geophysical surveys by allowing for precise adjustments in survey design based on the simulation outcomes.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.948
Threshold uncertainty score0.606

Codex and Gemma teacher scores by category

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

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 head0.050
GPT teacher head0.274
Teacher spread0.224 · 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 teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designSimulation or modeling
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
Published2024
Admission routes1
Has abstractyes

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