Silicate Liquid Immiscibility within the Crystal Mush: Evidence from Ti in Plagioclase from the Skaergaard Intrusion
A key target in the study of layered intrusions is to constrain the liquid line of descent of the magma. However, the evolution of the interstitial liquid is rarely considered, and its liquid line of descent is often assumed to be equivalent to that of the bulk magma. Because of extensive sub-solidu...
Main Author: | Humphreys, M |
---|---|
Format: | Journal article |
Language: | English |
Published: |
2011
|
Similar Items
-
Silicate Liquid Immiscibility within the Crystal Mush: Late-stage Magmatic Microstructures in the Skaergaard Intrusion, East Greenland
by: Holness, M, et al.
Published: (2011) -
Chemical Evolution of Intercumulus Liquid, as Recorded in Plagioclase Overgrowth Rims from the Skaergaard Intrusion
by: Humphreys, M
Published: (2009) -
Lateral reactive infiltration in avertical gabbroic crystal mush, skaergaard intrusion, east greenland
by: Namur, O, et al.
Published: (2013) -
Melt-rich segregations in the Skaergaard Marginal Border Series: Tearing of a vertical silicate mush
by: Humphreys, M, et al.
Published: (2010) -
Formation of transgressive anorthosite seams in the Bushveld Complex via tectonically induced mobilisation of plagioclase-rich crystal mushes
by: Wolfgang D. Maier, et al.
Published: (2016-11-01)