Abstract
We used in this study data recorded by two consecutive passive broadband deployments on the Gulf of Aden northern margin, Dhofar region, Sultanate of Oman. The objective of these deployments is to map the young eastern Gulf of Aden passive continental margin crust and upper mantle structure and rheology. In this study we use shear wave splitting analysis to map lateral variations of upper mantle anisotropy beneath the study area. We found in this study splitting magnitudes to vary between 0.33 and 1.0 s delay times, averaging about 0.6 s for a total of 17 stations from both deployment periods. Results show distinct abrupt lateral anisotropy variation along the study area. Three anisotropy zones are identified: a western zone dominated by NW–SE anisotropy orientations, an eastern zone dominated with NE–SW anisotropy orientations, and central zone with mixed anisotropy orientations similar to the east and west zones. We interpret these shorter wavelength anisotropy zones to possibly represent fossil lithospheric mantle anisotropy. We postulate that the central anisotropy zone may be representing a Precambrian–Cambrian suture zone that separates two terranes to the east and west of it. The anisotropy zones west and east, being used indicative of different terranes with different upper mantle anisotropy signature.
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Acknowledgment
The authors are grateful to all who have contributed directly or indirectly to this work. This work was supported by NERC grant NE/C514031/1 and a Royal Society travel grant to the first author. GDR Margins contribution.
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Al-Lazki, A. et al. (2013). Upper mantle anisotropy of Southeast Arabia passive margin [Gulf of Aden Northern conjugate margin], Oman. In: Al Hosani, K., Roure, F., Ellison, R., Lokier, S. (eds) Lithosphere Dynamics and Sedimentary Basins: The Arabian Plate and Analogues. Frontiers in Earth Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-30609-9_21
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DOI: https://doi.org/10.1007/978-3-642-30609-9_21
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