11 citations · 14 across the 4 of their papers we have counts for
6 papers · 1 filter
Magmatic intrusions control Io's crustal thickness
D. C. Spencer, R. F. Katz, I. J. Hewitt
Io, the most volcanically active body in the solar system, loses heat through eruptions of hot lava. Heat is supplied by tidal heating and is thought to be transferred through the…
Devolatilization of Subducting Slabs, Part II: Volatile Fluxes and Storage
Meng Tian, Richard Katz, David Rees Jones +1
Subduction is a crucial part of the long-term water and carbon cycling between Earth's exosphere and interior. However, there is broad disagreement over how much water and carbon i…
Devolatilization of Subducting Slabs, Part I: Thermodynamic Parameterization and Open System Effects
Meng Tian, Richard Katz, David Rees Jones
The amount of HO and CO that is carried into deep mantle by subduction beyond subarc depths is of fundamental importance to the deep volatile cycle but remains debated. Giv…
Consequences of glacial cycles for magmatism and carbon transport at mid-ocean ridges
Nestor G. Cerpa, David W. Rees Jones, Richard F. Katz
Magmatism and volcanism transfer carbon from the solid Earth into the climate system. This transfer may be modulated by the glacial/interglacial cycling of water between oceans and…
The melting column as a filter of mantle trace-element heterogeneity
Tong Bo, Richard F. Katz, Oliver Shorttle +1
The observed variability of trace-element concentration in basaltic lavas and melt inclusions carries information about heterogeneity in the mantle. The difficulty is to disentangl…
Modelling Coupled Oscillations of Volcanic CO2 Emissions and Glacial Cycles
Jonathan M. A. Burley, Peter Huybers, Richard F. Katz
Following the mid-Pleistocene transition, the dominant period of glacial cycles changed from 40 ka to ~100 ka. It is broadly accepted that the 40 ka glacial cycles were driven by c…