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Record W2026747567 · doi:10.1111/sed.12151

Reply to the Discussion by Schieber on “Mud dispersal across a Cretaceous prodelta: Storm‐generated, wave‐enhanced sediment gravity flows inferred from mudstone microtexture and microfacies” by Plint (), Sedimentology 61, 609–647

2014· article· en· W2026747567 on OpenAlexafffundabout
A. Guy Plint, Burns A. Cheadle

Bibliographic record

VenueSedimentology · 2014
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsWestern University
FundersNatural Sciences and Engineering Research Council of CanadaAmerican Association of Petroleum Geologists
KeywordsGeologySedimentologyCretaceousSedimentGeomorphologyOceanographyPaleontology

Abstract

fetched live from OpenAlex

SedimentologyVolume 62, Issue 1 p. 394-400 Discussion and Reply Reply to the Discussion by Schieber on "Mud dispersal across a Cretaceous prodelta: Storm-generated, wave-enhanced sediment gravity flows inferred from mudstone microtexture and microfacies" by Plint (†), Sedimentology 61, 609–647 A. Guy Plint, A. Guy Plint Department of Earth Sciences, University of Western Ontario, London, Ontario, N6A 5B7 CanadaSearch for more papers by this authorBurns A. Cheadle, Burns A. Cheadle Department of Earth Sciences, University of Western Ontario, London, Ontario, N6A 5B7 CanadaSearch for more papers by this author A. Guy Plint, A. Guy Plint Department of Earth Sciences, University of Western Ontario, London, Ontario, N6A 5B7 CanadaSearch for more papers by this authorBurns A. Cheadle, Burns A. Cheadle Department of Earth Sciences, University of Western Ontario, London, Ontario, N6A 5B7 CanadaSearch for more papers by this author First published: 22 July 2014 https://doi.org/10.1111/sed.12151Citations: 2Read the full textAboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onEmailFacebookTwitterLinkedInRedditWechat References Angiel, P.J. (2013) Allostratigraphy, sedimentology and paleogeography of the Cretaceous Upper Fort St. John Group (Upper Albian-Lower Cenomanian) in north-eastern British Columbia. Unpublished Ph.D. thesis, University of Western Ontario, 402 p. Cheadle, B.A. (2014a) Compaction state of aggregate grains in carbonaceous mudstones: evidence from microfabric studies of the Upper Cretaceous Colorado Group, Western Canada Foreland Basin. Oral presentation at AAPG Annual Convention and Exhibition: April 6–9 2014, Houston, TX. http://www.searchanddiscovery.com/abstracts/html/2014/90189ace/1841009.html Cheadle, B.A. (2014b) Redistribution of organomineralic aggregate grains in the Upper Cretaceous Second White Specks Formation, Western Canada Foreland Basin. Oral presentation at GeoConvention 2014: May 12–16 2014, Calgary, AB. http://www.geoconvention.com/uploads/abstracts/107_GC2014_Redistribution_of_Organomineralic_Aggregate_Grains.pdf Cheadle, B.A. and Jiang, P. (2013) Born this way – inherited heterogeneity and microporosity modalities in 'hydrid' reservoirs of the Upper Cretaceous Colorado Group, Western Canada Foreland Basin. Oral presentation at GeoConvention 2013, Calgary, May 6–10 2013. http://www.geoconvention.com/uploads/2013abstracts/056_GC2013_ Flynn, J. and Cheadle, B.A. (2014) Regional allostratigraphic correlations across a foreland basin: evidence for a tectonically- or eustatically-dominated system? Oral presentation at GeoConvention 2014: May 12–16 2014, Calgary, AB. http://www.geoconvention.com/uploads/abstracts/285_GC2014_Regional_allostratigraphic_correlations_across_a_foreland_basin.pdf Jiang, P. (2013) Pore morphometrics and thermal evolution of organic-matter microporosity, Colorado Group, Western Canada Foreland Basin. Unpublished M.Sc. thesis, University of Western Ontario, 231 p. Jiang, P. and Cheadle, B.A. (2013) Depositional and burial domain influences on microporosity modalities in carbonaceous mudstones of the Upper Cretaceous Colorado Group, Western Canada Foreland Basin (poster presentation). AAPG Annual Convention and Exhibition: May 19–22 2013, Pittsburgh, PA. http://www.searchanddiscovery.com/documents/2013/50802jiang/ndx_jiang.pdf Kalkreuth, W. and McMechan, M. (1988) Burial history and thermal maturity, Rocky Mountain Front Ranges, Foothills and Foreland, east-central British Columbia and adjacent Alberta. Am. Assoc. Petrol. Geol. Bull., 72, 1395–1410. Marion, K.P. (2014) Microstructure of Cretaceous mudrocks from a variety of depositional environments Unpublished B.Sc. thesis, University of Western Ontario, 70 p. Nishida, N., Ito, M., Inoue, A. and Takizawa, S. (2013) Clay fabric of fluid mud deposits from laboratory and field observations: potential application to the stratigraphic record. Mar. Geol., 337, 1–8. Plint, A.G. (2000) Sequence stratigraphy and paleogeography of a Cenomanian deltaic complex: the Dunvegan and lower Kaskapau formations in subsurface and outcrop, Alberta and British Columbia. Bull. Can. Petrol. Geol., 47, 43–79. Plint, A.G. (2014) Mud dispersal across a Cretaceous prodelta: storm-generated, wave-enhanced sediment gravity flows inferred from mudstone microtexture and microfacies. Sedimentology, 61, 609–647. Plint, A.G. and Macquaker, J.H.S. (2013) Reply to Discussion on: Shallow-water, storm-influenced sedimentation on a distal, muddy ramp: Upper Cretaceous Kaskapau Formation, Western Canada foreland basin. J. Sed. Res., 83, 1200–1201. Plint, A.G. and Nummedal, D. (2000) The falling stage systems tract: recognition and importance in sequence stratigraphic analysis. In: Sedimentary responses to forced regressions (Eds D. Hunt and R.L.G. Gawthorpe), Geol. Soc. London Spec. Pub., 172, 1–17. Plint, A.G. and Wadsworth, J.A. (2003) Sedimentology and palaeogeomorphology of four large valley systems incising delta plains, Western Canada Foreland Basin: implications for mid-Cretaceous sea-level changes. Sedimentology, 50, 1147–1186. Plint, A.G., Macquaker, J.H.S. and Varban, B.L. (2012) Shallow-water, storm-influenced sedimentation on a distal, muddy ramp: Upper Cretaceous Kaskapau Formation, Western Canada foreland basin. J. Sed. Res., 82, 801–822. Rylaarsdam, J.R., Varban, B.L., Plint, A.G., Buckley, L.G. and McCrea, R.T. (2006) Middle Turonian Dinosaur Paleoenvironments in the Kaskapau Formation, NE British Columbia. Can. J. Earth Sci., 43, 631–652. Schieber, J. (1998) Sedimentary features indicating erosion, condensation, and hiatuses in the Chattanooga Shale of central Tennessee: relevance for sedimentary and stratigraphic evolution. In: Shales and Mudstones, vol. 1 (Eds J. Schieber, W. Zimmerle and P. Sethi), pp. 187–215. E. Schweizerbart'sche Verlagsbuchhandlung (Nägele u. Obermiller), Stuttgart, Germany. Schieber, J. (2013) SEM observations in ion-milled samples of Devonian black shales from Indiana and New York: the petrographic context of multiple pore types. In: Electron microscopy of shale hydrocarbon reservoirs (Eds W. Camp, E. Diaz and B. Wawak), AAPG Mem. 102, 153–171. Schieber, J. and Bennett, R. (2013) Discussion on: Shallow-water, storm-influenced sedimentation on a distal, muddy ramp: Upper Cretaceous Kaskapau Formation, Western Canada foreland basin. J. Sed. Res., 83, 1198–1199. Schieber, J., Green, S., Suarez-Rivera, R. and Mastalrez, M. (2013) Textural and compositional heterogeneity of tight shales at the micro-scale (oral presentation). 47th US Rock Mechanics/Geomechanics Symposium: 23–26 June 2013, San Francisco, CA, USA. ARMA 13-366, American Rock Mechanics Association, Alexandria, VA, USA. https://www.onepetro.org/conference-paper/ARMA-2013-366 Citing Literature Volume62, Issue1January 2015Pages 394-400 ReferencesRelatedInformation

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)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.514
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.000
Science and technology studies0.0010.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.001
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 head0.009
GPT teacher head0.230
Teacher spread0.221 · 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".

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Citations2
Published2014
Admission routes3
Has abstractyes

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