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Record W1980071418 · doi:10.2113/econgeo.108.5.1119

The Long Canyon Deposit: Anatomy of a New Off-Trend Sedimentary Rock-Hosted Gold Discovery in Northeastern Nevada

2013· article· en· W1980071418 on OpenAlexaff
Moira T. Smith, D Rhys, K Ross, Christopher Lee, James N. Gray

Bibliographic record

VenueEconomic Geology · 2013
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsGeoscience BC
Fundersnot available
KeywordsGeologyBrecciaGeochemistryParagenesisSedimentary rockDolomitePyriteMarcasiteMineralogyMetamorphic rockSphalerite

Abstract

fetched live from OpenAlex

Abstract The Long Canyon deposit is a new sedimentary rock-hosted gold discovery located in northeastern Nevada, over 150 km east of the well-explored Carlin trend. Unlike most examples of this type, the deposit is hosted in a sequence of Cambro-Ordovician carbonate rocks deposited in a periodically emergent, platform to shelf-edge environment. The strata were strongly deformed and weakly metamorphosed during a mid-Mesozoic orogenic event that segmented and extended a brittle, 80-m-thick dolomite layer into a series of elongate, N- to NE-trending boudin blocks, while the enclosing limestone underwent ductile deformation. This unusual structural architecture focused subsequent contractional deformation, as well as Tertiary extensional brittle deformation, forming pathways for meteoric and hydrothermal fluids, which formed and enlarged dissolution cavities and dissolution breccias along boudin margins, boudin necks, and normal faults. Gold occurs primarily in zones of polyphase dissolution breccias that are localized in minor faults and fold hinges in the structurally complex areas along and adjacent to dolomite block margins. Two general phases of brecciation are present, including calcareous breccias and later, Fe ± As oxide-rich breccias, which carry the highest gold grades. Breccias are accompanied by variable pervasive silicification. Alteration assemblages include zoned dickite + white mica + hematite in the cores of mineralized zones, with peripheral kaolinite + sericite and goethite + hematite and, ultimately, more distal illite + smectite. Local preservation of fine-grained sulfides encapsulated in calcite and silica suggests that the iron oxide assemblages may represent oxidation of fine-grained pyrite + marcasite + arsenopyrite assemblages. As currently defined, the Long Canyon deposit extends for 3 km in a northeasterly direction and consists of several subparallel zones of mineralization focused on boudin block margins, boudin necks, and incipient boudins. It contains a combined (measured, indicated, and inferred) estimated resource comprising 2.2 million ounces of gold, at an average grade of ~2.3 g/t gold. Metallurgical work indicates that the deposit is highly amenable to cyanidation by heap leaching or milling. The Long Canyon deposit is open to further exploration and resource additions, and is shallowly buried, relatively high grade, and thoroughly oxidized. The stratigraphic position of the Long Canyon deposit on the Paleozoic shelf and its location well east of the majority of identified major trends indicate significant potential for new discoveries in this underexplored area of eastern Nevada.

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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.292
Threshold uncertainty score0.995

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)0.0060.001

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 head0.006
GPT teacher head0.183
Teacher spread0.178 · 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 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

Citations13
Published2013
Admission routes1
Has abstractyes

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