Melting the hydrous, subarc mantle: the origin of primitive andesites
AL Mitchell, TL Grove - Contributions to Mineralogy and Petrology, 2015 - Springer
This experimental study is the first comprehensive investigation of the melting behavior of an
olivine+ orthopyroxene±spinel—bearing fertile mantle (FM) composition as a function of …
olivine+ orthopyroxene±spinel—bearing fertile mantle (FM) composition as a function of …
Preferential formation of chlorite over talc during Si‐metasomatism of ultramafic rocks in subduction zones
Talc formation via silica‐metasomatism of ultramafic rocks is believed to play key roles in
subduction zone processes. Yet, the conditions of talc formation remain poorly constrained …
subduction zone processes. Yet, the conditions of talc formation remain poorly constrained …
A Log‐Ratio‐Based Algorithm for Petrologic Mass‐Balance Problems and Uncertainty Assessment
We provide a new algorithm for mass‐balance calculations in petrology and geochemistry
based on the log‐ratio approach championed initially by John Aitchison (eg, Aitchison …
based on the log‐ratio approach championed initially by John Aitchison (eg, Aitchison …
Melting of the primitive Martian mantle at 0.5–2.2 GPa and the origin of basalts and alkaline rocks on Mars
We have performed piston–cylinder experiments on a primitive martian mantle composition
between 0.5 and 2.2 GPa and 1160 to 1550° C. The composition of melts and residual …
between 0.5 and 2.2 GPa and 1160 to 1550° C. The composition of melts and residual …
Analysis and experimental investigation of Apollo sample 12032, 366‐18, a chemically evolved basalt from the Moon
AC Stadermann, BL Jolliff… - … & Planetary Science, 2022 - Wiley Online Library
Abstract Sample 12032, 366‐18 is a 41.2 mg basaltic rock fragment collected during the
Apollo 12 mission to the Moon. It is enriched in incompatible trace elements (eg, 7 ppm Th) …
Apollo 12 mission to the Moon. It is enriched in incompatible trace elements (eg, 7 ppm Th) …
Experimental calibration of an Fe3+/Fe2+-in-amphibole oxybarometer and its application to shallow magmatic processes at Shiveluch Volcano, Kamchatka
Oxygen fugacity is an important but difficult parameter to constrain for primitive arc magmas.
In this study, the partitioning behavior of Fe3+/Fe2+ between amphibole and glass …
In this study, the partitioning behavior of Fe3+/Fe2+ between amphibole and glass …
Melts of garnet lherzolite: experiments, models and comparison to melts of pyroxenite and carbonated lherzolite
Phase equilibrium experiments on a compositionally modified olivine leucitite from the
Tibetan plateau have been carried out from 2.2 to 2.8 GPa and 1,380–1,480° C. The …
Tibetan plateau have been carried out from 2.2 to 2.8 GPa and 1,380–1,480° C. The …
The quench control of water estimates in convergent margin magmas
Here we present a study on the quenchability of hydrous mafic melts. We show via
hydrothermal experiments that the ability to quench a mafic hydrous melt to a homogeneous …
hydrothermal experiments that the ability to quench a mafic hydrous melt to a homogeneous …
Experimentally determined effects of olivine crystallization and melt titanium content on iron isotopic fractionation in planetary basalts
Olivine is the most abundant mantle mineral at depths relevant to oceanic crust production
through melting. It is also a liquidus phase for a wide range of mafic and ultramafic magma …
through melting. It is also a liquidus phase for a wide range of mafic and ultramafic magma …
Origin of the Apollo 14, 15, and 17 yellow ultramafic glasses by mixing of deep cumulate remelts
We examine the fO 2-dependent melting conditions of the Apollo 14 yellow intermediate-Ti
ultramafic glasses and the melting processes that formed the full suite of lunar yellow …
ultramafic glasses and the melting processes that formed the full suite of lunar yellow …