Rayleigh^Taylor instabilities from hydration and melting propel 'cold plumes' at subduction zones
By Taras V. Gerya, D. Yuen. 2003
541 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/85462287dcbf8276399d00693a9488b6c8e844c4
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In Geophysics
Citations in the corpus
- Modeling the Dynamics of Subducting Slabs (2008, background): “…affects thermal structure of the slab and overriding plate (Bodri & Bodri 1978, Furukawa 1993, Eberle et al. 2002, van Keken et al. 2002, Honda & Saito 2003, Kneller et al. 2007), fluid migration in the wedge (Cagnioncle et al. 2007), and deformation of the overriding plate (Gerya & Yuen 2003).”
- Magmatic implications of mantle wedge plumes: Experimental study (2008, background): “1) (Gerya and Yuen, 2003; Gerya et al., 2004, 2006), active continental margins (Fig.”
- Subduction styles in the Precambrian: Insight from numerical experiments (2009, methodology): “…32 Ma, and after the beginning of subduction, melt-bearing subducted sediments detach from the slab and form a compositionally buoyant plume (e.g. Gerya and Yuen, 2003a; Gerya et al., 2006), whereas at λmelt=0.1, after 6Ma the subducted sediments start tomove below the continental lithosphere…”
- Transient hot channels: Perpetrating and regurgitating ultrahigh-pressure, high-temperature crust–mantle associations in collision belts (2008, methodology): “D code I2ELVIS (Gerya and Yuen, 2003a; Gerya and Yuen, 2007) based on finite-differences with a non-diffusive marker-in-cell technique used for advecting and updating material properties such as rock type, temperature, stress and plastic strain.”
- A model for C-O-H fluid in the Earth's mantle (2009, background): “…roles in most geologic processes like fluid– rock interactions (McCollom and Shock, 1998; Zheng et al., 1999), dehydration of subducted slabs (Gerya and Yuen, 2003; Spandler et al., 2003; Rupke et al., 2004), destruction of craton (Liu, 2005), metasomatism (Stalder 0016-7037/$ - see front…”
- Numerical modelling of spontaneous slab breakoff and subsequent topographic response (2011, methodology): “The numerical experiments were conducted in two dimensions using the thermo-mechanical code I2VIS (Gerya and Yuen, 2003a).”