Partitioning coefficients between olivine and silicate melts
JH Bédard - Lithos, 2005 - Elsevier
Variation of Nernst partition coefficients (D) between olivine and silicate melts cannot be
neglected when modeling partial melting and fractional crystallization. Published natural …
neglected when modeling partial melting and fractional crystallization. Published natural …
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 …
Rapid transition to long-lived deep crustal magmatic maturation and the formation of giant porphyry-related mineralization (Yanacocha, Peru)
M Chiaradia, D Merino, R Spikings - Earth and Planetary Science Letters, 2009 - Elsevier
The Yanacocha magmatic field (northern Peru) hosts the largest high sulfidation gold
deposit on Earth. Mineralization is associated with porphyritic intrusions distributed along a …
deposit on Earth. Mineralization is associated with porphyritic intrusions distributed along a …
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 …
Magmatic development of an intra-oceanic arc: High-precision U-Pb zircon and whole-rock isotopic analyses from the accreted Talkeetna arc, south-central Alaska
The accreted Talkeetna arc, south-central Alaska, is an archetypal example of an intra-
oceanic arc crustal section. Arc-related units include all levels of a lithospheric column, from …
oceanic arc crustal section. Arc-related units include all levels of a lithospheric column, from …
[HTML][HTML] Magmatic crystal records in time, space, and process, causatively linked with volcanic unrest
MJ Pankhurst, DJ Morgan, T Thordarson… - Earth and Planetary …, 2018 - Elsevier
How a volcano has behaved throughout its past is a guide to its future behaviour. Detailed
knowledge of what preceded eruptions from specific volcanoes, and how this can be …
knowledge of what preceded eruptions from specific volcanoes, and how this can be …
Trace element partitioning coefficients between silicate melts and orthopyroxene: parameterizations of D variations
JH Bédard - Chemical Geology, 2007 - Elsevier
Nernst partition coefficient data between orthopyroxene and silicate melts show variability
for most trace elements which cannot be neglected when designing petrogenetic trace …
for most trace elements which cannot be neglected when designing petrogenetic trace …
Open-system magma chamber evolution: an energy-constrained geochemical model incorporating the effects of concurrent eruption, recharge, variable assimilation …
FJ Spera, WA Bohrson - Journal of Petrology, 2004 - academic.oup.com
Significant petrogenetic processes governing the geochemical evolution of magma bodies
include magma R echarge (including formation of 'quenched inclusions' or enclaves) …
include magma R echarge (including formation of 'quenched inclusions' or enclaves) …
The magmatic architecture of continental flood basalts I: Observations from the Deccan Traps
Flood basalts are some of the largest magmatic events in Earth history, with intrusion and
eruption of millions of km3 of basaltic magma over a short time period (∼ 1–5 Ma). A typical …
eruption of millions of km3 of basaltic magma over a short time period (∼ 1–5 Ma). A typical …