Pre-existing oblique transfer zones and transfer/transform relationships in continental margins: New insights from the southeastern Gulf of Aden, Socotra Island, Yemen

Transfer zones are ubiquitous features in continental rifts and margins, as are transform faults in oceanic lithosphere. Here, we present a structural study of the Hadibo Transfer Zone (HTZ), located in Socotra Island (Yemen) in the southeastern Gulf of Aden. There, we interpret this continental tra...

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Bibliographic Details
Published in:Tectonophysics 2013-11, Vol.607, p.32-50
Main Authors: Bellahsen, N., Leroy, S., Autin, J., Razin, P., d'Acremont, E., Sloan, H., Pik, R., Ahmed, A., Khanbari, K.
Format: Article
Language:English
Subjects:
Classification
Divergence
Earth Sciences
Environmental Sciences
Faults
Fracture mechanics
Fracture zone
Global Changes
Gulfs
Islands
Marine
Oblique rifting
Sciences of the Universe
Segmentation
Spreading
Structural inheritance
Tectonics
Transfer fault zone
Transform fault
Transforms
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Summary:Transfer zones are ubiquitous features in continental rifts and margins, as are transform faults in oceanic lithosphere. Here, we present a structural study of the Hadibo Transfer Zone (HTZ), located in Socotra Island (Yemen) in the southeastern Gulf of Aden. There, we interpret this continental transfer fault zone to represent a reactivated pre-existing structure. Its trend is oblique to the direction of divergence and it has been active from the early up to the latest stages of rifting. One of the main oceanic fracture zones (FZ), the Hadibo–Sharbithat FZ, is aligned with and appears to be an extension of the HTZ and is probably genetically linked to it. Comparing this setting with observations from other Afro-Arabian rifts as well as with passive margins worldwide, it appears that many continental transfer zones are reactivated pre-existing structures, oblique to divergence. We therefore establish a classification system for oceanic FZ based upon their relationship with syn-rift structures. Type 1 FZ form at syn-rift structures and are late syn-rift to early syn-OCT. Type 2 FZ form during the OCT formation and Type 3 FZ form within the oceanic domain, after the oceanic spreading onset. The latter are controlled by far-field forces, magmatic processes, spreading rates, and oceanic crust rheology. •Study of pre-existing oblique transfer faults in the Gulf of Aden continental margin•Comparison with other Afro-Arabian rifts•Classification of oceanic F.Z. based on their relationships with syn-rift structures•Segmentation of the Gulf of Aden
ISSN:0040-1951
1879-3266
DOI:10.1016/j.tecto.2013.07.036