Ultralow velocity zone and deep mantle flow beneath the Himalayas are linked to a subducted slab
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Publisher
Springer Science and Business Media LLC
Link
https://www.nature.com/articles/s41561-024-01387-4.pdf
Reference5 articles.
1. Hansen, S. E., Garnero, E. J., Li, M., Shim, S.-H. & Rost, S. Globally distributed subducted materials along the Earth’s core–mantle boundary: implications for ultralow velocity zones. Sci. Adv. 9, eadd4838 (2023). This paper presents an interesting hypothesis for the origin of ULVZs.
2. McNamara, A. K., Garnero, E. J. & Rost, S. Tracking deep mantle reservoirs with ultra-low velocity zones. Earth Planet. Sci. Lett. 299, 1–9 (2010). A review of geodynamic evidence for how mantle convection might influence ULVZs.
3. Yu, S. & Garnero, E. J. Ultralow velocity zone locations: a global assessment. Geochem. Geophys. Geosyst. 19, 396–414 (2018). This review discusses the global distribution of ULVZs.
4. Cottaar, S. & Romanowicz, B. An unsually large ULVZ at the base of the mantle near Hawaii. Earth Planet. Sci. Lett. 355–356, 213–222 (2012). This paper introduces the modelling of ULVZs using Sdiff postcursors.
5. Wolf, J., Long, M. D., Creasy, N. & Garnero, E. On the measurement of Sdiff splitting caused by lowermost mantle anisotropy. Geophys. J. Int. 233, 900–921 (2023). This paper introduces the technique that we have used to infer lowermost mantle deformation.
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