Diffusion in pyroxene, mica and amphibole
DJ Cherniak, A Dimanov - Reviews in Mineralogy and …, 2010 - pubs.geoscienceworld.org
This chapter presents an overview of diffusion data for pyroxenes, amphiboles and micas.
These minerals are grouped together since amphiboles and micas are closely related in …
These minerals are grouped together since amphiboles and micas are closely related in …
A new clinopyroxene-liquid barometer, and implications for magma storage pressures under Icelandic rift zones
DA Neave, KD Putirka - American Mineralogist, 2017 - degruyter.com
Pressure is one of the key variables that controls magmatic phase equilibria. However,
estimating magma storage pressures from erupted products can be challenging. Various …
estimating magma storage pressures from erupted products can be challenging. Various …
Crystallization of the lunar magma ocean and the primordial mantle-crust differentiation of the Moon
We present crystallization experiments on silicate melt compositions related to the lunar
magma ocean (LMO) and its evolution with cooling. Our approach aims at constraining the …
magma ocean (LMO) and its evolution with cooling. Our approach aims at constraining the …
The role of pyroxenite in basalt genesis: Melt‐PX, a melting parameterization for mantle pyroxenites between 0.9 and 5 GPa
S Lambart, MB Baker, EM Stolper - Journal of Geophysical …, 2016 - Wiley Online Library
Geochemical and isotopic data suggest that the source regions of oceanic basalts may
contain pyroxenite in addition to peridotite. In order to incorporate the wide range of …
contain pyroxenite in addition to peridotite. In order to incorporate the wide range of …
Experimental determination of C, F, and H partitioning between mantle minerals and carbonated basalt, CO2/Ba and CO2/Nb systematics of partial melting, and the …
A Rosenthal, EH Hauri, MM Hirschmann - Earth and Planetary Science …, 2015 - Elsevier
To determine partitioning of C between upper mantle silicate minerals and basaltic melts, we
executed 26 experiments between 0.8 and 3 GPa and 1250–1500° C which yielded 37 …
executed 26 experiments between 0.8 and 3 GPa and 1250–1500° C which yielded 37 …
Mineralogical heterogeneities in the Earth's mantle: Constraints from Mn, Co, Ni and Zn partitioning during partial melting
The first-row transition elements (FRTEs) are compatible to moderately incompatible during
melting in mafic and ultramafic systems. Unlike highly incompatible elements, FRTEs are …
melting in mafic and ultramafic systems. Unlike highly incompatible elements, FRTEs are …
The beginnings of hydrous mantle wedge melting
This study presents new phase equilibrium data on primitive mantle peridotite (0.33 wt% Na
2 O, 0.03 wt% K 2 O) in the presence of excess H 2 O (14.5 wt% H 2 O) from 740 to 1,200° C …
2 O, 0.03 wt% K 2 O) in the presence of excess H 2 O (14.5 wt% H 2 O) from 740 to 1,200° C …
Clinopyroxene–liquid equilibria and geothermobarometry in natural and experimental tholeiites: the 2014–2015 Holuhraun eruption, Iceland
Clinopyroxene–liquid geothermobarometry is a widely used tool for estimating the
conditions under which mafic magmas are stored before they erupt. However, redox …
conditions under which mafic magmas are stored before they erupt. However, redox …
Research governance: regulating risk and reducing harm?
Risk assessment can be thought of as the lens through which we anticipate the
consequences of research and the impact of the actions of researchers. The way in which …
consequences of research and the impact of the actions of researchers. The way in which …
Experimentally determined mineral/melt partitioning of first-row transition elements (FRTE) during partial melting of peridotite at 3 GPa
Ratios of first-row transition elements (FRTE), such as Fe/Mn and Zn/Fe, may be fractionated
differently by partial melting of peridotite than by partial melting of recycled lithologies like …
differently by partial melting of peridotite than by partial melting of recycled lithologies like …