activity
20152019
most citedThe role of volatiles in reactive melt transport in the asthenosphere

158 citations · 494 across the 7 of their papers we have counts for

collaborators

7 papers

physics.geo-ph2019★ 6 cited

Periodic outgassing as a result of unsteady convection in Ray Lava Lake, Mount Erebus, Antarctica

Janine Birnbaum, Tobias Keller, Jenny Suckale +1

Persistently active lava lakes show continuous outgassing and open convection over years to decades. Ray Lake, the lava lake at Mount Erebus, Ross Island, Antarctica, maintains lon…

physics.geo-ph2018★ 88 cited

A continuum model of multi-phase reactive transport in igneous systems

Tobias Keller, Jenny Suckale

Multi-phase reactive transport processes are ubiquitous in igneous systems. A challenging aspect of modelling igneous phenomena is that they range from solid-dominated porous to li…

physics.flu-dyn2018★ 27 cited

Bistability of buoyancy-driven exchange flows in vertical tubes

Jenny Suckale, Zhipeng Qin, Davide Picchi +2

Buoyancy-driven exchange flows are common to a variety of natural and engineering systems ranging from persistently active volcanoes to counterflows in oceanic straits. Experiments…

astro-ph.EP2018★ 47 cited

Magma ascent in planetesimals: control by grain size

Tim Lichtenberg, Tobias Keller, Richard F. Katz +2

Rocky planetesimals in the early solar system melted internally and evolved chemically due to radiogenic heating from Al-26. Here we quantify the parametric controls on magma genes…

physics.geo-ph2017★ 26 cited

Magmatic focusing to mid-ocean ridges: the role of grain size variability and non-Newtonian viscosity

Andrew J Turner, Richard F Katz, Mark D Behn +1

Melting beneath mid-ocean ridges occurs over a region that is much broader than the zone of magmatic emplacement to form the oceanic crust. Magma is focused into this zone by later…

physics.geo-ph2016★ 142 cited

Volatiles beneath mid-ocean ridges: deep melting, channelised transport, focusing, and metasomatism

Tobias Keller, Richard F Katz, Marc M Hirschmann

Deep-Earth volatile cycles couple the mantle with near-surface reservoirs. Volatiles are emitted by volcanism and, in particular, from mid-ocean ridges, which are the most prolific…