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Hydrocarbon Potential of the Mississippian Carbonate Platform, Bechar Basin, Algerian Sahara

2000· article· en· W2113849081 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

VenueAAPG Bulletin · 2000
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geophysical Studies Worldwide
Canadian institutionsCentre de Géomatique du QuébecGeological Survey of CanadaUniversité Laval
Fundersnot available
KeywordsGeologyCarbonateStructural basinGeochemistryCarbonate platformHydrocarbon explorationPaleontologyGeomorphologyMining engineeringFacies

Abstract

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Abstract The western Bechar basin contains a 1500-2000-m-thick Mississippian succession of carbonates consisting of superposed shoaling-upward sequences, whose porosity or diagenesis have never been investigated to establish the reservoir potential of these carbonates. In this paper, we present a diagenetic and porosity evolution of the Visean part of the Mississippian carbonate platform that may lead to the development of new exploration fairways in the region. A diagenetic model is proposed in which ooid and crinoid grainstones may have a reservoir potential if hydrocarbon migration occurred before the end of the Serpukhovian, prior to complete occlusion of porosity. The two facies investigated are Waulsortian-type buildups and overlying ooid and crinoid grainstones that form regularly alternating packages in the thick upper Visean succession. The diagenetic sequence contains five calcite cement phases (C1-C5) that were investigated for isotope geochemistry and fluid inclusion microthermometry. The isotopic signatures of calcite cements range from marine for C1 to deeper burial environments for the 18O-depleted C3 and C4. Fluid inclusion data indicate that C3 and C4 (60-80% of the total cement) precipitated from hot, saline basinal fluids, whereas a meteoric-phreatic origin is suggested for C5. Temperatures of cementation, inferred from stable oxygen isotopes and homogenization temperatures of fluid inclusions, indicate that most pores within the buildups (shelter, stromatactoid, moldic, breccia, and vuggy) were occluded after only a few hundred meters of burial. In contrast, pores in the ooid and crinoid grainstones (mainly interparticle) stayed open after thousands of meters (900-2500 m) of burial. We hypothesize that these grainstones may have served as a regional conduit for hydrocarbon migration from the basin to the carbonate platform. Basin subsidence rate ranged from 220 m/m.y. during the Visean to 40 m/m.y. during the Serpukhovian-Bashkirian, which suggests that 20 m.y. was needed to fill most porosity. As a result, the western Bechar limestones can be considered a good target for petroleum exploration if the hydrocarbon migration occurred before the end of the Serpukhovian. This conclusion has important implications because the Mississippian limestones lie directly above potential Upper Devonian source rock in the Bechar basin.

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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 categoriesInsufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.778
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
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)0.0330.001

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.

Opus teacher head0.005
GPT teacher head0.159
Teacher spread0.154 · 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