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Enregistrement 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 sur OpenAlexafffundabout
A. Guy Plint, Burns A. Cheadle

Notice bibliographique

RevueSedimentology · 2014
Typearticle
Langueen
DomaineEarth and Planetary Sciences
ThématiqueGeological formations and processes
Établissements canadiensWestern University
Organismes subventionnairesNatural Sciences and Engineering Research Council of CanadaAmerican Association of Petroleum Geologists
Mots-clésGeologySedimentologyCretaceousSedimentGeomorphologyOceanographyPaleontology

Résumé

récupéré en direct d'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

Récupéré en direct depuis OpenAlex et désinversé. Les résumés ne sont pas conservés dans cette base de données : les index inversés représentent 8,6 Go des 9,3 Go de texte de la base, et le serveur dispose de 13 Go libres.

Comment cette classification a été obtenuedéplier

Prédiction distillée sur la base complète

Imitation des enseignants

Ni prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.

score de la tête « metaresearch » (Codex)0,001
score de la tête « metaresearch » (Gemma)0,000
Version: codex-gemma-dda1882f352aStatut de validation: machine_predicted_unvalidated
Catégories candidatesMéta-épidémiologie (sens strict)
Catégories consensuellesaucune
DomaineSignal candidat: aucune · Signal consensuel: aucune
Devis d'étudeSignal candidat: Sans objet · Signal consensuel: Sans objet
GenreSignal candidat: Empirique · Signal consensuel: Empirique
Score de désaccord entre enseignants0,514
Score d'incertitude au seuil1,000

Scores Codex et Gemma par catégorie

CatégorieCodexGemma
Métarecherche0,0010,000
Méta-épidémiologie (sens strict)0,0000,000
Méta-épidémiologie (sens large)0,0010,000
Bibliométrie0,0000,000
Études des sciences et des technologies0,0010,000
Communication savante0,0000,000
Science ouverte0,0000,000
Intégrité de la recherche0,0000,001
Charge utile insuffisante (le modèle a refusé de juger)0,0010,000

Scores machine (provisoires)

Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.

Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.

Tête enseignante Opus0,009
Tête enseignante GPT0,230
Écart entre enseignants0,221 · la distance entre les deux têtes enseignantes sur ce seul travail
Statut de validationscore_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découle

Classification

machine, non validée

Prédiction automatique; un appel candidat d’une seule tête enseignante, pas un consensus.

Devis d'étudeSans objet
Domainenon disponible
GenreEmpirique

Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».

En bref

Citations2
Publié2014
Routes d'admission3
Résumé présentoui

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