Peperite : processes and products of magma-sediment mingling
Bibliographic record
Abstract
Research Papers: Peperite - a review of magma-sediment mingling, I.P. Skilling et al. Water/magma interaction - some theory and experiments on peperite formation, K. Wohletz Dynamic mingling of magma and liquefied sediments, B. Zimanowski, R. Buttner Characteristics and origin of peperite involving coarse-grained host sediment, R.J. Squire, J. McPhie Magma composition and viscosity as controls on peperite texture - an example from Passamaquoddy Bay, southeastern Canada, K.A. Dadd, N.A. Van Wagoner Middle Miocene volcaniclastic dikes at Kukedo, Shimane Peninsula, SW Japan - fluidization of volcaniclastic beds by emplacement of syn-volcanic andesitic dikes, K. Kano Peperite as a record of early-stage phreatomagmatic fragmentation processes - an example from the Hopi Buttes volcanic field, Navajo Nation, Arizona, USA, J.A. Hooten, M.H. Ort On the formation of deep-seated subterranean peperite-like magma-sediment mixtures, V. Lorenz et al. Rhyolitic globular peperites from the Aznalcollar mining district, (Iberian Pyrite Belt, Spain) - physical and chemical controls, T. Donaire et al. Melting and mingling of phonolitic pumice deposits with intruding dykes - an example from the Otago Peninsula, New Zealand, U. Martin, J.D.L. White Morphology of a crater-filling lava lake margin, The Peninsula tuff cone, Tule Lake National Wildlife Refuge, California - implications for formation of peperite textures, A. Lavine, K.R. Aalto Peperitic textures of Ordovician dacitic synsedimentary intrusions in Argentina's Puna Highland - clues to emplacement conditions, B. Coira, B. Perez Pumiceous rhyolitic peperite in ancient submarine volcanic successions, C.C. Gifkins et al. Granulation of weak rock as a precursor to peperite formation - coal peperite, Coombs Hills, Antarctica, M.K. McClintock, J.D.L. White Textural evidence of peperites inside pillow lavas at Acicastello Castle Rock, Mt. Etna, Sicily), R.A. Corsaro, P. Mazzoleni Lava-sediment interaction in desert settings are all peperite-like textures the result of magma-water interaction?, D.A. Jerram, H. Stollhofen.
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 machine prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.001 | 0.000 |
| Meta-epidemiology (broad) | 0.001 | 0.000 |
| Bibliometrics | 0.003 | 0.003 |
| Science and technology studies | 0.001 | 0.001 |
| Scholarly communication | 0.002 | 0.003 |
| Open science | 0.001 | 0.001 |
| Research integrity | 0.001 | 0.001 |
| Insufficient payload (model declined to judge) | 0.002 | 0.001 |
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.
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 source (direct Gemma or distilled Codex), 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".