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The life cycle of large igneous provinces
Extremely voluminous magmatic systems known as large igneous provinces (LIPs)
punctuate Earth's history, and the gases they release plausibly link large-scale geodynamic …
punctuate Earth's history, and the gases they release plausibly link large-scale geodynamic …
Pyroclastic density currents: state of the art and perspectives
Pyroclastic density currents (PDCs) are mixtures of two components, namely solid particles
and fluid (gas) phase. They macroscopically behave as dense, multiphase gravity currents …
and fluid (gas) phase. They macroscopically behave as dense, multiphase gravity currents …
Quantum magmatism: Magmatic compositional gaps generated by melt-crystal dynamics
Compositional gaps are common in volcanic series worldwide. The pervasive generation of
compositional gaps influences the mechanical and thermal properties of the crust, and holds …
compositional gaps influences the mechanical and thermal properties of the crust, and holds …
Trace element indicators of crystal accumulation in silicic igneous rocks
If fractional crystallization coupled with some crustal assimilation (AFC) is the dominant
process for generating evolved magmas in the Earth's crust, large quantities of igneous …
process for generating evolved magmas in the Earth's crust, large quantities of igneous …
The fluid mechanics of pyroclastic density currents
Pyroclastic density currents are generated in explosive volcanic eruptions when gas and
particle mixtures remain denser than the surrounding atmosphere. These mobile currents …
particle mixtures remain denser than the surrounding atmosphere. These mobile currents …
Homogenization processes in silicic magma chambers by stirring and mushification (latent heat buffering)
Heterogeneities in crustal magma chambers are generated by incomplete mixing of different
batches of magmas, precipitation or remelting of solids~ 10–20% denser than surrounding …
batches of magmas, precipitation or remelting of solids~ 10–20% denser than surrounding …
On the kinematics and dynamics of crystal‐rich systems
Partially molten rocks, often called a mush, are examples of a hydrogranular mixture where
the dynamics are controlled by both fluid and crystal‐crystal interactions. An obstacle to …
the dynamics are controlled by both fluid and crystal‐crystal interactions. An obstacle to …
Rift-related transition from andesite to rhyolite volcanism in the Taupo Volcanic Zone (New Zealand) controlled by crystal–melt dynamics in mush zones with variable …
Abstract The Taupo Volcanic Zone (TVZ), located in the North Island of New Zealand,
represents part of a magmatic arc that is at present undergoing active extension. Around 0· 9 …
represents part of a magmatic arc that is at present undergoing active extension. Around 0· 9 …
Coupling of turbulent and non-turbulent flow regimes within pyroclastic density currents
Volcanic eruptions are at their most deadly when pyroclastic density currents sweep across
landscapes to devastate everything in their path,. The internal dynamics underpinning these …
landscapes to devastate everything in their path,. The internal dynamics underpinning these …
Inside pyroclastic density currents–uncovering the enigmatic flow structure and transport behaviour in large-scale experiments
Pyroclastic density currents (PDCs) are the most lethal threat from volcanoes. While there
are two main types of PDCs (fully turbulent, fully dilute pyroclastic surges and more …
are two main types of PDCs (fully turbulent, fully dilute pyroclastic surges and more …