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 …
[图书][B] Using geochemical data: to understand geological processes
HR Rollinson, H Rollinson, V Pease - 2021 - books.google.com
This textbook is a complete rewrite, and expansion of Hugh Rollinson's highly successful
1993 book Using Geochemical Data: Evaluation, Presentation, Interpretation. Rollinson and …
1993 book Using Geochemical Data: Evaluation, Presentation, Interpretation. Rollinson and …
Crustal melting vs. fractionation of basaltic magmas: Part 1, granites and paradigms
Granitoids are a major component of the continental crust. They play a pivotal role in its
evolution, either by adding new material (continental growth), or by reworking older …
evolution, either by adding new material (continental growth), or by reworking older …
Combined thermodynamic–geochemical modeling in metamorphic geology: boron as tracer of fluid–rock interaction
M Konrad-Schmolke, R Halama - Lithos, 2014 - Elsevier
Quantitative geochemical modeling is today applied in a variety of geological environments
from the petrogenesis of igneous rocks to radioactive waste disposal. In addition, the …
from the petrogenesis of igneous rocks to radioactive waste disposal. In addition, the …
Trace element indicators of crystal accumulation in silicic igneous rocks
CD Deering, O Bachmann - Earth and Planetary Science Letters, 2010 - Elsevier
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 …
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 …
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 …
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 …
Trace element partitioning coefficients between terrestrial silicate melts and plagioclase feldspar: Improved and simplified parameters
JH Bédard - Geochimica et Cosmochimica Acta, 2023 - Elsevier
Nernst partition coefficient data are compiled and parameterized against commonly
measured and petrologically significant Input Variables, allowing plagioclase/melt D values …
measured and petrologically significant Input Variables, allowing plagioclase/melt D values …