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Record W4415777358 · doi:10.2118/229595-ms

Stratigraphic and Sedimentological Characterization of An Unconventional Carbonate Deposit: An Example from the Late Cretaceous Shilaif Formation, United Arab Emirates

2025· article· W4415777358 on OpenAlexaff
Greg M. Baniak, Christian Abaco, Nathan E. Leonard, Dana B.K. Kinnaird, Walid Kholeif, Fatimah Rosly

Bibliographic record

Venuenot available
Typearticle
Language
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsAlberta EnergyPetro-Canada
Fundersnot available
KeywordsFaciesCarbonateCarbonate platformSedimentary depositional environmentCretaceousForaminiferaCarbonate rockEcological successionStage (stratigraphy)

Abstract

fetched live from OpenAlex

Abstract The Late Cretaceous (Cenomanian) Shilaif Formation is an unconventional oil deposit located in the Emirate of Abu Dhabi in western United Arab Emirates (UAE). Presently, it is undergoing early-stage appraisal drilling and development. Due to the reservoir in its natural state having a very low permeability (well below 1mD), traditional primary recovery techniques cannot be used. Instead, extraction of the oil will occur via hydraulic fracking of the reservoir. To better optimize landing zone placement of horizontal wells, which in turn will help lead to improved design of the wells, operations require a thorough understanding of the depositional fabric and stratigraphic architecture of the reservoir. The Shilaif Formation represents a deep-marine carbonate succession deposited within an intrashelf basin. Using Arabian Plate boundary nomenclature present in offsetting wells from various offsetting countries, three primary sequences can be delineated (from oldest to youngest): K120 (Lower), K130 (Middle), and K140 (Upper). Each of these three sequences can be further sub-divided into lowstand (LST), transgressive (TST), highstand (HST), and falling stage (FSST) systems tracts and their corresponding parasequence sets. At the core level, massive bedded and bioturbated organic-rich carbonate facies in each of the three sequences frequently correspond with TST and early stage HST successions. Thin-sections reveal significant planktonic foraminifera and calcispheres. Biostratigraphic analysis of core samples suggests much of the organic material is a by-product of phytoplankton (algal) blooms. Conversely, massive bedded and bioturbated non-organic carbonate core facies in each of the three sequences commonly correspond with FSST and LST successions. Thin-section analysis reveals a higher abundance of fossiliferous fragments thus indicating sediment transport from adjacent platform margins into the basin. It must be noted that different combinations of these organic and non-organic facies, however, can occur within various systems tracts and therefore underpins the need to do detailed core logging and subsequent correlation across the field. Finally, many key stratigraphic surfaces are punctuated by examples of Glossifungities ichnofacies and their recognition in core are of critical importance towards building the basin model and understanding water benches.

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 imitation

Not 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.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.079
Threshold uncertainty score0.158

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0030.002
Science and technology studies0.0010.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
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 head0.026
GPT teacher head0.230
Teacher spread0.204 · 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 source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
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

Citations0
Published2025
Admission routes1
Has abstractyes

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