Detrital zircon U-Pb and (U-Th)/He geochronology of the central Morondava Basin, Madagascar
Notice bibliographique
Résumé
Formation of the Phanerozoic basins of Madagascar coincided with the initial stages of Permian break-up of Gondwana. The sources of the sediments in these basins are from the seven major Precambrian terranes that border them. The tectonic history of rifting, drifting, and uplift of the Madagascan terrane over the last 300 million years is recorded within the sedimentary strata that comprise the Morondava Basin, the largest of these basins located along the west coast. In this study, we have applied detrital zircon U-Pb geochronology and (U-Th)/He low-temperature thermochronology to resolve the sedimentation patterns and thermal history of the Morondava Basin as Madagascar separated from Africa and subsequently India. Nine coarse-grained siliciclastic samples were taken along two transects parallel to the Morondava River in the central Morondava Basin. Karoo sandstones and shales were deposited directly atop the basement during Permo-Triassic rifting. Two samples from each transect were taken in the uppermost Jurassic Karoo sandstones. Overlying the Karoo are carbonates that were deposited as part of a carbonate platform as the basin experienced Middle Jurassic subsidence due to successful rifting during the separation of Madagascar and Africa. A Late Jurassic unconformity suggests tectonic quiescence. As the passive margin subsidence renewed, changes in eustatic sea level resulted in several cycles of sedimentation, and two Cretaceous samples in each transect were collected from this interval. Separation of India from Madagascar during the Turonian resulted in uplift of the central highlands and tilting of the Morondava Basin accompanied by extensive volcanic activity throughout the basin. Previously published apatite fission track studies mark this as the final stage of cooling. Above a Paleocene unconformity, deposition occurred in the Eocene with a package of sandstones and shales represented by a single sample in the southern transect. The detrital zircon U-Pb age distributions include common Neoarchean and Neoproterozoic populations which suggests input from the basement terranes of the Madagascan central highlands (Antananarivo domain). A subset of samples contain a Paleo- to Mesoarchean population linked to the metasedimentary Anosyen domain and a Cambrian population associated with metamorphic zircon formed during the Pan-African Orogeny the source of which occurs in the southwestern basement terranes. Spatial variations within the detrital zircon U-Pb age populations indicate two distinct sedimentation patterns separating the north and south parts of the basin and a likely post-Jurassic sediment recycling history within the Morondava Basin. Initial zircon (U-Th)/He ages range from 500 to 80 Ma with effective uranium (eU) values ranging from 35 to 1760, which exhibit a strong negative eU-age relationship and indicate partial resetting of zircon throughout the basin. The combined data will be utilized to construct the low-temperature thermal history of the basin.
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Comment cette classification a été obtenuedéplier
Prédiction machine sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Le volet Gemma est une étiquette directe du modèle pour chaque travail de la base, lue sur la notice réduite au titre. Le volet Codex est un classifieur appris des 10 348 étiquettes directes de Codex et calibré sur les taux pondérés de l'échantillon; les champs sans appui suffisant ne portent aucun appel Codex. Le mode candidate est l'union des deux volets; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont pas des étiquettes humaines.
Scores du classifieur distillé par catégorie (deux têtes)
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,000 | 0,000 |
| Méta-épidémiologie (sens strict) | 0,000 | 0,000 |
| Méta-épidémiologie (sens large) | 0,000 | 0,000 |
| Bibliométrie | 0,001 | 0,001 |
| Études des sciences et des technologies | 0,001 | 0,000 |
| Communication savante | 0,000 | 0,000 |
| Science ouverte | 0,000 | 0,000 |
| Intégrité de la recherche | 0,000 | 0,000 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,001 | 0,000 |
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.
score_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 découleClassification
machine, non validéePrédiction automatique; un appel candidat d’une seule source (Gemma direct ou Codex distillé), pas un consensus.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».