The Samail subduction zone dilemma: Geochronology of high-pressure rocks from the Saih Hatat window, Oman, reveals juxtaposition of two subduction zones with …
Abstract The Samail Ophiolite in the Oman Mountains formed at a Cretaceous subduction
zone that was part of a wider Neo-Tethys plate-boundary system. The original configuration …
zone that was part of a wider Neo-Tethys plate-boundary system. The original configuration …
[HTML][HTML] Structural architecture and Late Cretaceous exhumation history of the Saih Hatat Dome (Oman), a review based on existing data and semi-restorable cross …
Abstract The Saih Hatat Dome in the Al Hajar Mountains provides an outstanding
opportunity to study subduction/exhumation processes coeval with obduction of the Semail …
opportunity to study subduction/exhumation processes coeval with obduction of the Semail …
Oligocene/Early Miocene E/W‐Shortening in the Oman Mountains Related to Oblique Arabia‐India Convergence
Field survey, literature review, geological map interpretation, GPlates reconstruction and LA‐
ICP‐MS U‐Pb dating of synkinematic calcite demonstrate that∼ E/W‐shortening in eastern …
ICP‐MS U‐Pb dating of synkinematic calcite demonstrate that∼ E/W‐shortening in eastern …
Thermal maturity of the Hawasina units and origin of the Batinah Mélange (Oman Mountains): Insights from clay minerals
Abstract The Oman Mountains developed during Cretaceous to Cenozoic time by obduction
of the Semail Ophiolite on top of the Arabian rifted margin. The tectonic pile of the orogenic …
of the Semail Ophiolite on top of the Arabian rifted margin. The tectonic pile of the orogenic …
Uplift dynamics of the obducted northeastern continental margin of the Arabian Peninsula, Sultanate of Oman
Eustatic sea level changes and vertical tectonic movements are producing uplifted
paleoshorelines. Along subduction zones, uplifted terraces are used to study fault activities …
paleoshorelines. Along subduction zones, uplifted terraces are used to study fault activities …
Post-obduction listwaenite genesis in the Oman Mountains inferred from structural analysis and U-Pb carbonate dating
Listwaenite, a distinctive rock formed by carbonation of peridotite, is important for
understanding carbon fluxes and storage in the deep Earth. In northern Oman, this lithology …
understanding carbon fluxes and storage in the deep Earth. In northern Oman, this lithology …
Lagoonal Microfacies, Lithostratigraphy, Correlation and Shale Migration of the Basal Middle Eocene Seeb Formation (Rusayl Embayment, Sultanate of Oman)
The study improves the understanding of the basal part of the Eocene Seeb Formation of
Oman, informally known as “Unit 1”, in terms of microfacies, lithostratigraphy and shale …
Oman, informally known as “Unit 1”, in terms of microfacies, lithostratigraphy and shale …
Chapter 2 Tectonostratigraphy of the eastern part of the Oman Mountains
This chapter provides comprehensive descriptions of 52 numbered formations/rock units of
the Southeastern Oman Mountains, based on available literature. The oldest eight …
the Southeastern Oman Mountains, based on available literature. The oldest eight …
Lithospheric evolution of eastern Arabia based on surface wave and receiver function analyses
The geodynamic evolution of Eastern Arabia comprises three major events that must have
acted on the entire lithosphere below the present-day passive continental margin. Starting …
acted on the entire lithosphere below the present-day passive continental margin. Starting …
[HTML][HTML] The complex continental margin of NE Oman: Fault-gouge dating of the Wadi Kabir Fault at the northern margin of the Saih Hatat window, Sultanate of Oman …
The complex structural geometry along the northern continental margin of Oman formed
during polyphase deformation from the late Cretaceous to the Miocene. We focus on the …
during polyphase deformation from the late Cretaceous to the Miocene. We focus on the …