Short time scales of magmatic assimilation from diffusion modeling of multiple elements in olivine
Open-system processes have a large capacity to modify magma compositions during differentiation. Obtaining the rates of such processes is essential to understanding and constraining the evolution of magmatic systems. Here we quantify the time scales for magmatic assimilation of hydrous mafic to ultr...
Main Authors: | Costa, Fidel, Dungan, Michael |
---|---|
Other Authors: | School of Physical and Mathematical Sciences |
Format: | Journal Article |
Language: | English |
Published: |
2012
|
Subjects: | |
Online Access: | https://hdl.handle.net/10356/95062 http://hdl.handle.net/10220/8720 |
Similar Items
-
Lithium diffusion in olivine records magmatic priming of explosive basaltic eruptions
by: Lynn, Kendra J., et al.
Published: (2020) -
Magmatic Na-rich phlogopite in a suite of gabbroic crustal xenoliths from Volcán San Pedro, Chilean Andes : evidence for a solvus relation between phlogopite and aspidolite
by: Costa, Fidel, et al.
Published: (2012) -
How do olivines record magmatic events? Insights from major and trace element zoning
by: de Maisonneuve, Caroline Bouvet, et al.
Published: (2017) -
DIPRA : a user-friendly program to model multi-element diffusion in olivine with applications to timescales of magmatic processes
by: Girona, Társilo, et al.
Published: (2013) -
Diffusion chronometry and the timescales of magmatic processes
by: Costa, Fidel, et al.
Published: (2020)