Geological, fluid-chemical and petrochronological studies of the East Kemptville Sn(-Cu-Zn-Ag-In) deposit and its Devonian host batholith (Nova Scotia, Canada).
Bibliographic record
Abstract
Primary tin ores form in magmatic-hydrothermal systems related to highly-evolved granites \nenriched in lithophile elements (e.g., Li, Cs, Rb, U). Causative magmas are sourced from melting \n(or contamination by) enriched crust, or from melting hydrothermally-altered mantle. These \ngranites form in large, multi-phase complexes (batholiths) and concentrate tin through fractional \ncrystallization. The latter increases volatiles (H2O, F) in residual melts that are emplaced at \nshallow crustal depths, and thus the hydrothermal component to Sn-systems. Volatiles exsolve \ninto aqueous fluids that contain soluble Sn2+. These fluids typically separate into highly-saline \nbrines and vapours, and precipitate ore (SnO2) via oxidation of the Sn2+ \n. The fluids focus along \nfractures in the crust and their accumulation is dependent on fluid- versus lithostatic pressures. The northern Appalachian evolution included incremental emplacement of numerous batholiths \nand tin occurrences. The largest of these is the South Mountain Batholith (SMB) in Nova Scotia, \nwhich was emplaced deep in the crust; although is host to multiple evolved granites, the SMB \ncontains only one significant tin deposit at East Kemptville (EK). To establish the depositional \nsetting of EK at a greater crustal depth, this thesis analyses its geology and fluid chemistry as \nwell as stable (O) and radiogenic (Re-Os, U-Pb, Lu-Hf) isotopes for both EK mineralization and \nthe zircon minerals that represent the SMB. The study addresses the absence of other significant \ntin deposits in the SMB by evaluating the source of metal endowment. \nDue to its deep emplacement, the fluids at EK show no evidence of phase separation, yet \nabundant evidence of pressure-cycling. The latter allowed for replenishment of ore fluids during \ndeposit formation; whereas initial tin formed via fluid-rock exchange, later ores formed from mixing with foreign fluids. This segmented hydrothermal evolution at EK is reflected by a \nrange of mineralization ages. \nThe zircon ages and chemistry indicate: 1) the SMB formed over 15-20 m.y. from altered mantle \nmelts that underwent contamination by host rocks; and 2) the EK host is temporally and \nisotopically distinct from the SMB, and likely evolved from a lower crust-derived melt. The \ndistinct source suggests other tin occurrences in the region share a similar origin.
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How this classification was reachedexpand
Full frame distilled prediction
Teacher imitationNot 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.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.001 | 0.000 |
| Bibliometrics | 0.000 | 0.001 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.001 |
| Insufficient payload (model declined to judge) | 0.001 | 0.000 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one teacher head, not a consensus.
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".