Consequences of viscous anisotropy in a deforming, two-phase aggregate. Why is porosity-band angle lowered by viscous anisotropy?
Takei, Y Katz, R (17 Jun 2015) doi:10.48550/arxiv.1506.05286
Devolatilization of Subducting Slabs, Part I: Thermodynamic Parameterization and Open System Effects
Tian, M Katz, R Jones, D (06 Jun 2019) doi:10.48550/arxiv.1906.02819
Devolatilization of Subducting Slabs, Part II: Volatile Fluxes and Storage
Tian, M Katz, R Jones, D May, D (08 Jun 2019) doi:10.48550/arxiv.1906.03473
Tidal controls on the lithospheric thickness and topography of Io from magmatic segregation and volcanism modelling
Spencer, D Katz, R Hewitt, I (20 Aug 2020) doi:10.48550/arxiv.2008.09022
Magmatic channelisation by reactive and shear-driven instabilities at mid-ocean ridges: a combined analysis
Jones, D Zhang, H Katz, R (31 Aug 2020) doi:10.48550/arxiv.2008.13674
Volatility forecasting with machine learning and intraday commonality
Zhang, C Zhang, Y Cucuringu, M Qian, Z (01 Jan 2022) doi:10.2139/ssrn.4022147
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