| Titre | Soft-sediment deformation structures in alkaline lake deposits of Lower Permian Fengcheng Formation, Junggar Basin, NW China: implications for syn-sedimentary tectonic activity |
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| Auteur | Tang, W B; Zhang, Y Y; Pe-Piper, G; Piper, D J W ; Guo, Z; Li, W |
| Source | Sedimentary Geology vol. 406, 105719, 2020 p. 1-19, https://doi.org/10.1016/j.sedgeo.2020.105719 |
| Image |  |
| Année | 2020 |
| Séries alt. | Ressources naturelles Canada, Contribution externe 20200098 |
| Éditeur | Elsevier B.V. |
| Document | publication en série |
| Lang. | anglais |
| DOI | https://doi.org/10.1016/j.sedgeo.2020.105719 |
| Media | papier; en ligne; numérique |
| Formats | pdf; html |
| Lat/Long OENS | 80.0000 100.0000 50.8333 40.5000 |
| Sujets | Permien inférieur; milieux tectoniques; crevasses; bassins; déformation; formation de failles; milieu sédimentaire; milieux lacustres; structures sédimentaires; sismicité; secousses séismiques;
paléogéographie; lithofaciès; cônes alluviaux; deltas; géologie des dépôts meubles/géomorphologie; tectonique; sédimentologie; Sciences et technologie; Nature et environnement; Phanérozoïque; Paléozoïque; Permien |
| Illustrations | cartes de localisation; cartes géolscientiques généralisées; diagrammes stratigraphiques; profils; coupes lithologiques; tableaux; coupes transversales; photographies; coupes de corrélation;
modèles |
| Diffusé | 2020 07 02 |
| Résumé | (disponible en anglais seulement)
Soft-sediment deformation structures (SSDS) are an important tool for interpreting paleoseismicity and depositional environments in ancient basin successions.
The northwestern margin of Junggar Basin is a key region for understanding the paleogeography and basin attributes of the Junggar Basin during the early Permian. In the Lower Permian (Kungurian) Fengcheng Formation, nine lithofacies are grouped into
fan delta, fluvial delta, and shallow, deep and alkaline lacustrine facies associations. Vertical transitions of the sedimentary environments show that the lake basin experienced expansion during deposition of the Lower (P1f1) and Middle (P1f2)
members and the shrinkage during the Upper Member (P1f3), which is consistent with the paleogeographic distribution of lithofacies in different members. Conventional cores show a wide variety of SSDS, including ductile (folds, convolute lamination,
and load structures), hybrid ductile-brittle, and brittle deformation structures (microfaults, breccias, boudinage and sedimentary dikes). SSDS mainly occurred in a still and deep lacustrine environment. These deformation structures were not formed
in any specific lacustrine environment, as there is no difference with the undeformed sedimentary units of the same sedimentary facies. Thus, the triggering mechanism is interpreted as intermittent earthquakes. Lake expansion under arid condition and
SSDS intervals with vertical repetition and possible lateral continuity indicate that most seismicity was during the Middle member (P1f2), corresponding with the main activity on basin-bounding normal faults. The enhanced faulting at this time
generated accommodation, creating lacustrine conditions in the basin depocenter. It is thus clear that the early Permian Mahu sag represents an active rift basin with bounding faults, and is not a foreland basin. |
| Sommaire | (Résumé en langage clair et simple, non publié)
Des distributions de structures créées par des secousses sismiques dans des sédiments de lacs anciens donnent des preuves de l'évolution
géologique d'un bassin de rift riche en pétrole. Les concepts s'appliquent directement au groupe de Horton dans le Canada atlantique. |
| GEOSCAN ID | 326375 |
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