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Record W2790821716 · doi:10.4095/261783

Drift isopach, till isopach, and till facies reconstructions for Northwest Territories and northern Yukon

2010· report· en· W2790821716 on OpenAlexaffabout
I R Smith, K Lesk-Winfield

Bibliographic record

Venuenot available
Typereport
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsNatural Resources Canada
Fundersnot available
KeywordsIsopach mapGeologyRadiocarbon datingGeomorphologyFaciesArchaeologyPaleontologyGeography

Abstract

fetched live from OpenAlex

Unconsolidated sediments, collectively referred to as "drift," blanket much of the terrain in the Mackenzie corridor, Mackenzie Delta and adjoining regions of petroleum exploration and development in Northwest Territories and northern Yukon. The drift cover is dominantly till, but may also include significant regional and localized accumulations of glaciofluvial, glaciolacustrine, and glaciomarine sediments as well as post-, and pre-glacial-aged fluvial, lacustrine and aeolian deposits. In places the drift cover can be 10s of metres thick. The sedimentology, thickness, composition, and compaction of the drift cover fundamentally influence much of the biological, hydrological, permafrost, and geomorphic characteristics of the landscape. Understanding the drift cover is thus recognized as being a key component of infrastructure development design and assessment, drift geochemical mineral and ore deposit exploration, and of particular relevance to all manner of ecological studies.This study principally uses seismic shothole drillers' logs (~275,000), collected during auger drilling of shotholes (10-40 m deep) to create cumulative drift isopach (thickness) models and derivative till isopach models. Transparencies of these two isopach models, overlaid onto a digital elevation model, depict areas of both positive constructional relief, and areas where drift has infilled valleys and/or blanketed the underlying topography. Differences and regional trends of drift and till thickness can be linked to compressional and extensional dynamics of glacial entrainment and deposition, and areas where glaciers impounded the regional drainage, into which sedimentation was focused.Further in aid of drift prospecting exploration, this study presents an identification of different till facies. Understanding of till facies is important because different facies are associated with either changes in glacial flow direction, and hence, bedrock source material, or can be used to characterize tills comprised of more locally derived bedrock material such as typically shale-rich basal "blue tills" found in the southeastern and central Mackenzie corridor, compared to overlying "brown tills" which are comprised of more far travelled, englacially transported Canadian Shield derived materials, deposited by deglacial lodgement and meltout processes. Understanding which till is being sampled during surface sediment collection, and hence, which types and locations of bedrock the sediments have been derived from, is critically important to the interpretation of drift geochemical analytical results.

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: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.738
Threshold uncertainty score0.966

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 studies0.0010.000
Scholarly communication0.0000.000
Open science0.0000.000
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 head0.031
GPT teacher head0.233
Teacher spread0.202 · 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 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

Citations7
Published2010
Admission routes2
Has abstractyes

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