The thickness of the crystal mush on the floor of the Bushveld magma chamber [PDF]
The thickness of the crystal mush on magma chamber floors can be constrained using the offset between the step-change in the median value of dihedral angles formed at the junctions between two grains of plagioclase and a grain of another phase (typically clinopyroxene, but also orthopyroxene and olivine) and the first appearance or disappearance of the
Marian Holness +2 more
exaly +11 more sources
Crystal scavenging from mush piles recorded by melt inclusions [PDF]
The increasingly prevalent view of magmatic systems as mush-dominated challenges the common assumption that melt inclusions record the pre-eruptive storage and processing of the melts they were erupted with.
Penny E. Wieser +4 more
doaj +19 more sources
Mesoscale and microscopic structures record compaction and crystal-melt segregation in silicic mushes [PDF]
Gravitationally-driven compaction has been proposed as an important mechanism for crystal-melt segregation in silicic mushes. However, there is no microstructural evidence of crystal deformation consistent with compaction in silicic plutonic rocks.
Yun-Chao Liu, Yao-Hui Jiang, Bo-Ning Han
doaj +4 more sources
Crystal Resorption as a Driver for Mush Maturation: an Experimental Investigation [PDF]
Abstract The thermal state of a magma reservoir controls its physical and rheological properties: at storage temperatures close to the liquidus, magmas are dominated by melt and therefore mobile, while at lower temperatures, magmas are stored as a rheologically locked crystal network with interstitial melt (crystal mush).
Martin F Mangler +7 more
openaire +4 more sources
The mechanical response of a magma chamber with poroviscoelastic crystal mush [PDF]
Improved understanding of the impact of crystal mush rheology on the response of magma chambers to magmatic events is critical for better understanding crustal igneous systems with abundant crystals. In this study, we extend an earlier model by (Liao et al, 2018) which considers the mechanical response of a magma chamber with poroelastic crystal mush ...
Yang liao +3 more
openaire +5 more sources
Numerical simulations of the mingling caused by a magma intruding a resident mush [PDF]
Currently, our ability to interpret the mechanics of magma mingling and mixing is limited by an incomplete understanding of the modes of mixing across all melt fractions and compositions.
Alexandre Carrara +2 more
doaj +2 more sources
The permeability of magma mush [PDF]
Models for the evolution of magma mush zones are of fundamental importance for understanding magma storage, differentiation in the crust, and melt extraction processes that prime eruptions.
Bretagne, Eloise Marie
core +6 more sources
The Surface Deformation Signature of a Transcrustal, Crystal Mush‐Dominant Magma System
AbstractThe transcrustal, mush‐dominated magma storage paradigm, which posits liquid melt is heterogeneously distributed within a vertically extensive magma mush, differs significantly from classical geodetic models, where melt is stored within liquid‐dominant chambers within an elastic crust.
Benjamin Mullet, Paul Segall
openaire +2 more sources
Consequences of a crystal mush-dominated magma plumbing system: a mid-ocean ridge perspective [PDF]
Johan Lissenberg +2 more
exaly +2 more sources
Lithium mica clasts document magmatic evolution prior to eruption in the macusani volcanic field in peru [PDF]
Typically found in rare-metal granites and pegmatites, lithium micas are increasingly considered a resource for lithium as global demand surges. In a recently discovered major lithium resource within the Macusani Volcanic Field in Peru, lithium mica ...
Lisard Torró +13 more
doaj +2 more sources

