[HTML][HTML] Morphology and controls of the mountain-front fan systems of the Hajar Mountains, south-east Arabia
Mountain-front fans are an important part of the global sediment system, acting as buffers
and stores of sediment between upland sources and down-system sinks. Fans emanate …
and stores of sediment between upland sources and down-system sinks. Fans emanate …
Assessing the robustness of geochronological records from the Arabian Peninsula: A new synthesis of the last 20 ka
The timing and extent of Late Quaternary climate and environmental changes in the Arabian
Peninsula were critical for human demographic changes. High resolution palaeoclimate …
Peninsula were critical for human demographic changes. High resolution palaeoclimate …
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 …
A 3-D crustal shear wave velocity model and Moho map below the Semail Ophiolite, eastern Arabia
C Weidle, L Wiesenberg, A El-Sharkawy… - Geophysical Journal …, 2022 - academic.oup.com
SUMMARY The Semail Ophiolite in eastern Arabia is the largest and best-exposed slice of
oceanic lithosphere on land. Detailed knowledge of the tectonic evolution of the shallow …
oceanic lithosphere on land. Detailed knowledge of the tectonic evolution of the shallow …
Postobductional kinematic evolution and geomorphology of a major regional structure—The Semail Gap Fault Zone (Oman Mountains)
Abstract The Semail Gap/Semail Gap Fault Zone is one of the most prominent tectonic
features in the Oman Mountains and is located between the Jabal Akhdar Dome in the west …
features in the Oman Mountains and is located between the Jabal Akhdar Dome in the west …
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 …
Structure of the offshore obducted Oman margin: Emplacement of Semail ophiolite and role of tectonic inheritance
The northern Oman margin is a key area for understanding the emplacement of the Semail
Ophiolite and obduction processes in general. This study uses a grid of 2D‐multichannel …
Ophiolite and obduction processes in general. This study uses a grid of 2D‐multichannel …
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 …
Ophiolites and ocean plate stratigraphy (OPS) preserved across the Central Mongolian Microcontinent: a new mega-archive of data for the tectonic evolution of the …
Following the breakup of Rodinia and the opening of the Paleo-Asian ocean the relative
positions of geological units (now in Mongolia) remain uncertain, and in consequence …
positions of geological units (now in Mongolia) remain uncertain, and in consequence …