Silicic magma reservoirs in the Earth's crust
O Bachmann, C Huber - American Mineralogist, 2016 - degruyter.com
Magma reservoirs play a key role in controlling numerous processes in planetary evolution,
including igneous differentiation and degassing, crustal construction, and volcanism. For …
including igneous differentiation and degassing, crustal construction, and volcanism. For …
Oxygen isotopes in mantle and crustal magmas as revealed by single crystal analysis
I Bindeman - Reviews in Mineralogy and Geochemistry, 2008 - pubs.geoscienceworld.org
Oxygen is the most abundant element in the Earth's crust, mantle, and fluids and therefore its
isotopic composition provides robust constraints on magma genesis. Application of oxygen …
isotopic composition provides robust constraints on magma genesis. Application of oxygen …
A model for eruption frequency of upper crustal silicic magma chambers
W Degruyter, C Huber - Earth and Planetary Science Letters, 2014 - Elsevier
Whether a magma body is able to produce eruptions and at what frequency remains a
challenging problem in volcanology as it involves the nonlinear interplay of different …
challenging problem in volcanology as it involves the nonlinear interplay of different …
Short time scales of magmatic assimilation from diffusion modeling of multiple elements in olivine
F Costa, M Dungan - Geology, 2005 - pubs.geoscienceworld.org
Open-system processes have a large capacity to modify magma compositions during
differentiation. Obtaining the rates of such processes is essential to understanding and …
differentiation. Obtaining the rates of such processes is essential to understanding and …
Thermo-mechanical reactivation of locked crystal mushes: Melting-induced internal fracturing and assimilation processes in magmas
Thermal reactivation of locked crystal mushes in the upper crust is a fundamental step
towards volcanic eruptions of crystal-rich magmas. Models of such reactivation events …
towards volcanic eruptions of crystal-rich magmas. Models of such reactivation events …
Multistage evolution of dolerites in the Karoo large igneous province, Central South Africa
ER Neumann, H Svensen, CY Galerne… - Journal of …, 2011 - academic.oup.com
Early Jurassic sheet-like intrusions (sills and dykes) are abundant in the Karoo Basin in
South Africa, and were emplaced as a part of the Karoo Large Igneous Province. Here we …
South Africa, and were emplaced as a part of the Karoo Large Igneous Province. Here we …
Thermodynamic model for energy-constrained open-system evolution of crustal magma bodies undergoing simultaneous recharge, assimilation and crystallization …
The Magma Chamber Simulator quantifies the impact of simultaneous recharge,
assimilation and crystallization through mass and enthalpy balance in a multicomponent …
assimilation and crystallization through mass and enthalpy balance in a multicomponent …
Cumulate formation and melt extraction from mush-dominated magma reservoirs: the melt flush process exemplified at mid-ocean ridges
M Boulanger, L France - Journal of Petrology, 2023 - academic.oup.com
Volcanism is the surface expression of extensive magmatic systems, with their intrusive
counterpart representing~ 80% of the total magma budget. Our knowledge of igneous …
counterpart representing~ 80% of the total magma budget. Our knowledge of igneous …
Differentiation of tholeiitic basalt to A-type granite in the Sept Iles layered intrusion, Canada
Abstract The undeformed 564 Ma Sept Iles layered intrusion (Quebec, Canada) is a large
igneous body of c. 20 000 km3. From the base to the top, it consists of a Layered Series …
igneous body of c. 20 000 km3. From the base to the top, it consists of a Layered Series …
Diagnosing open-system magmatic processes using the Magma Chamber Simulator (MCS): part II—trace elements and isotopes
Abstract The Magma Chamber Simulator (MCS) is a thermodynamic model that computes
the phase, thermal, and compositional evolution of a multiphase–multicomponent system of …
the phase, thermal, and compositional evolution of a multiphase–multicomponent system of …