Thrusting and veining under blueschist facies conditions: multi-technique and multiscalar study of the Little Snake Gorge Thrust, Jabal Akhdar Mountains (Oman)

Sanguettoli, Tommaso ; Sanguettoli, Tommaso (2025) Thrusting and veining under blueschist facies conditions: multi-technique and multiscalar study of the Little Snake Gorge Thrust, Jabal Akhdar Mountains (Oman). [Laurea magistrale], Università di Bologna, Corso di Studio in Geologia e territorio [LM-DM270]
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Abstract

The Oman Mountains are a complex orogenic system shaped by diverse tectonic events, serving as a natural observatory for studying subduction and obduction. Historically, the Jabal Akhdar Dome, a prominent tectonic window located in their central-eastern sector, was thought to have undergone only low-grade metamorphism, unaffected by deep subduction during the Cretaceous. However, recent discoveries challenge this view. Evidence of Cretaceous blueschist-facies metamorphism indicates high-pressure, low-temperature conditions typical of subduction channels. Studies in the “Little Snake Gorge” area have yielded new structural and metamorphic data, prompting a reassessment of the dome’s evolution. Deformation structures linked to the “Little Snake Gorge Thrust,” along with metamorphic aragonite in foliation-parallel veins, support a Cretaceous high-pressure overprint, likely tied to Late Cretaceous subduction of the Arabian margin beneath Eurasia. Subduction caused complex folding in Precambrian rocks, with alternating brittle and ductile phases. Structural data reveal deformation styles associated with high-pressure metamorphism. To define metamorphic conditions, Raman Spectroscopy on Carbonaceous Material (RSCM) was used, yielding peak conditions of ~348 ± 50 °C and 0.85 ± 0.12 GPa in the Mu’aydin Formation footwall. A model of progressive deformation, based on U-Pb geochronology, describes the evolution of the Little Snake Gorge Thrust, highlighting stress-axis rotation during Late Cretaceous subduction. The deformation history includes an initial SW-NE layer-parallel shortening, followed by folding and thrusting under blueschist conditions, and a final NNW-SSE folding phase linked to stress-field rotation, forming the interference structures observed today. These results enhance understanding of high-pressure metamorphism and support revising tectonometamorphic models for the Jabal Akhdar Dome.

Abstract
Tipologia del documento
Tesi di laurea (Laurea magistrale)
Autore della tesi
Sanguettoli, Tommaso ; Sanguettoli, Tommaso
Relatore della tesi
Correlatore della tesi
Scuola
Corso di studio
Indirizzo
CURRICULUM C: RAW MATERIALS EXPLORATION AND SUSTAINABILITY
Ordinamento Cds
DM270
Parole chiave
Oman,Oman Mountains,Jabal Akhdar Dome,Little Snake Gorge,Blueschists facies,Thrusting,Veining,Metamorphism,High-pressure metamorphism,Raman spectroscopy,RSCM,Aragonite,Blueschists,Subduction,Graphite,Carbonaceous material,Organic matter,Brittle,Ductile,Deformation,Brittle-ductile deformation,Hajir Formation,Mu'aydin Formation
Data di discussione della Tesi
24 Luglio 2025
URI

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