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Record W4408484013 · doi:10.5194/egusphere-egu25-20438

Reservoir characterization of a mixed siliciclastic-carbonate succession, Middle Cretaceous, southeastern Iraq

2025· preprint· en· W4408484013 on OpenAlexaff
Min Gao, Domenico Chiarella, Han Haiying, Chaozhong Ning, Zhou Lyu

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geophysical Studies
Canadian institutionsPetro-Canada
Fundersnot available
KeywordsSiliciclasticEcological successionCretaceousCarbonateGeologyMiddle EastGeochemistryPetrologyPaleontologyGeographyArchaeologyChemistrySedimentary depositional environmentEcology

Abstract

fetched live from OpenAlex

Mixed siliciclastic-carbonate deposits accumulated in the passive continental margin of the Arabian plate are commonly found in the Mesozoic stratigraphic interval in southeastern Iraq. As important hydrocarbon reservoirs in the area, the Cretaceous strata have attracted great interests of researchers to study their sedimentary features, depositional processes and petrophysical properties. However, in-depth studies considering the systematic evolution of a mixed siliciclastic-carbonate succession in the context of sequence stratigraphy and its control on the petrophysical properties of the rocks are still rare. In this study, two representative formations (i.e., the Nahr Umr and the Mishrif formations) that constitute a seismic-scale strata mixing (sensu Chiarella et al., 2017) were fully investigated. An integrated dataset, including core and thin section descriptions, well logs, and results from core experiments (e.g., XRD analysis, grain size distribution, porosity, and permeability measurements), was employed to perform a detailed analysis of sedimentary facies, interpret depositional environments, and evaluate petrophysical properties. The Nahr Umr Formation is dominated by siliciclastic sediments with sedimentary facies interpreted as distributary channel, tidal channel, tidal flat, tide-modified mouth bar, bay, lower shoreface, offshore transition and offshore. The assemblage of sedimentary structures observed in this formation, including cross-bedding, ripple cross-lamination, lenticular bedding, and wavy bedding, indicates a tide-influenced deltaic environment. This interpretation is further supported by the bimodal grain size distribution revealed through analysis, reflecting the combined influences of fluvial and tidal processes. The Mishrif Formation is dominated by carbonate sediments deposited in a carbonate platform environment, with sedimentary facies interpreted as high-energy shoal, low-energy shoal, tidal channel, lagoon, subtidal, swamp and incised valley. Local depositional environments transitioned among open platform, semi-restricted platform, and platform margin settings in response to relative sea-level fluctuations. The petrophysical properties of the studied formations are influenced by both sedimentary and diagenetic processes. High-quality reservoirs are typically associated with sedimentary facies such as distributary channels, tidal channels, and bioclastic shoals. Diagenetic dissolution has played an important role in enhancing reservoir quality.

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)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.024
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.028
GPT teacher head0.220
Teacher spread0.192 · 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 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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