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Record W6890230638 · doi:10.34944/dspace/7708

COMBINED STRUCTURAL ANALYSIS OF CORE AND IMAGE LOG OF TGH MB 76-31 EAST OF MOUNT BAKER, WASHINGTON STATE

2022· other· en· W6890230638 on OpenAlexaboutno aff

Bibliographic record

VenueTUScholarShare (Temple University) · 2022
Typeother
Languageen
Field
Topic
Canadian institutionsnot available
Fundersnot available
KeywordsVolcanoGeothermal gradientFracture (geology)Impact craterElectrical conduitBasaltAndesiteProspectingPorosityTemperature gradient

Abstract

fetched live from OpenAlex

Despite active volcanism, few geothermal energy resources have been developed in the Cascades Range. Temperature Gradient Hole (TGH) MB 76-31 was drilled to approximately 440 m measured depth to probe for zones where fractures provide fluid conduits that transport deep volcanic heat to shallow depths that could support baseload, carbon neutral electrical generation. These zones were predicted by a Play Fairway assessment (PFA) of resource potential along a zone 11 km west-southwest of the summit of Mount Baker Volcano, Washington State. Rock core, temperature logs, and an acoustic image log were obtained. By comparison to outcrops, the core is interpreted as the Chilliwack Group, comprised of partially metamorphosed basaltic to andesitic volcanics, but due to similar physical and mineral composition may represent the Nooksack Formation. Mapping of core reveals complex, steeply dipping networks of fractures and brecciation along slickensided strike slip faults; clay alteration is common in many of these structures. Most fractures are thoroughly healed by layers of chlorite and calcite, whereas chlorites and vermiculite line open fractures. Fracture porosity is primarily hosted by very dense fractures a few centimeters or less in length. These small fractures are not clearly evident or interpretable in image logs, leading to under-estimated fracture density and secondary porosity, although the image log provides good insights into frequency and attitude of fractures that fully transect the core. The combination of complex, non-planar fracture zones containing many short fractures and healing promote misinterpretation of natural fracture attitude and density in the image log. The equilibrated measured temperature reaches a maximum temperature 32°C at 408 m measured depth along a conductive gradient of 64ºC/km and calculated heat flow of 145 mW/m2 which is more than twice the regional average of 30ºC/km. The presence of vermiculite and several chlorite minerals lining fractures is consistent with the conductive temperature gradient measured in the well below a shallow isothermal zone, although, several fractures are open or only partially healed and resulted in fluid entries into the well. Together, the temperature gradient and vermiculite formation in the fractures indicate local influence of the Mt Baker magmatic system at the Little Park Creek TGH site and that TGH MB 76-31 reaches the upper edge of a caprock above a much deeper hydrothermal system. Do you conclude that this site will/will not support electrical generation? Should have a sentence here describing this since you start your abstract with the idea that you’re testing viability.

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 categoriesMeta-epidemiology (narrow), Insufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.496
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0020.001
Bibliometrics0.0070.006
Science and technology studies0.0000.001
Scholarly communication0.0000.001
Open science0.0010.001
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0190.000

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 head0.024
GPT teacher head0.240
Teacher spread0.217 · 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.

Study designNot applicable
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
Published2022
Admission routes1
Has abstractyes

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