WATER, MELTING, AND THE DEEP EARTH H2O CYCLE
MM Hirschmann - Annu. Rev. Earth Planet. Sci., 2006 - annualreviews.org
Hydrous melting driven by changes in H2O storage capacity may occur in a variety of
settings in the mantle, including in oceanic basalt sources and in deeper regions above and …
settings in the mantle, including in oceanic basalt sources and in deeper regions above and …
[HTML][HTML] Long-term Phanerozoic global mean sea level: Insights from strontium isotope variations and estimates of continental glaciation
Global mean sea level is a key component within the fields of climate and oceanographic
modelling in the Anthropocene. Hence, an improved understanding of eustatic sea level in …
modelling in the Anthropocene. Hence, an improved understanding of eustatic sea level in …
Serpentine and the subduction zone water cycle
This study explores a chemo-thermo-dynamic subduction zone model that solves for slab
dehydration during subduction. We investigate how changes in the incoming plate's …
dehydration during subduction. We investigate how changes in the incoming plate's …
Dehydration melting at the top of the lower mantle
The high water storage capacity of minerals in Earth's mantle transition zone (410-to 660-
kilometer depth) implies the possibility of a deep H2O reservoir, which could cause …
kilometer depth) implies the possibility of a deep H2O reservoir, which could cause …
Whole-mantle convection and the transition-zone water filter
D Bercovici, S Karato - Nature, 2003 - nature.com
Because of their distinct chemical signatures, ocean-island and mid-ocean-ridge basalts are
traditionally inferred to arise from separate, isolated reservoirs in the Earth's mantle. Such …
traditionally inferred to arise from separate, isolated reservoirs in the Earth's mantle. Such …
Linked magma ocean solidification and atmospheric growth for Earth and Mars
LT Elkins-Tanton - Earth and Planetary Science Letters, 2008 - Elsevier
Early in terrestrial planet evolution energetic impact, radiodecay, and core formation may
have created one or more whole or partial silicate mantle magma oceans. The time to …
have created one or more whole or partial silicate mantle magma oceans. The time to …
Partitioning of water during melting of the Earth's upper mantle at H2O-undersaturated conditions
EH Hauri, GA Gaetani, TH Green - Earth and Planetary Science Letters, 2006 - Elsevier
We present the results of an experimental study of the partitioning of water between common
upper mantle minerals (olivine, orthopyroxene, clinopyroxene, garnet) and silicate melt …
upper mantle minerals (olivine, orthopyroxene, clinopyroxene, garnet) and silicate melt …
Recent advances and perspectives of fluorite and perovskite-based dual-ion conducting solid oxide fuel cells
High-temperature solid-state electrolyte is a key component of several important
electrochemical devices, such as oxygen sensors for automobile exhaust control, solid oxide …
electrochemical devices, such as oxygen sensors for automobile exhaust control, solid oxide …
Water transport into the deep mantle and formation of a hydrous transition zone
E Ohtani, K Litasov, T Hosoya, T Kubo… - Physics of the Earth and …, 2004 - Elsevier
The phase relations in the peridotite–water system to the top of the lower mantle reveal that
a certain amount of water can be transported and stored in the transition zone by various …
a certain amount of water can be transported and stored in the transition zone by various …
Ultrahigh-pressure minerals and metamorphic terranes–the view from China
Ultrahigh-pressure (UHP) metamorphism refers to mineralogical modifications of continental
and oceanic crustal protoliths±associated mafic-ultramafic rocks initially formed or emplaced …
and oceanic crustal protoliths±associated mafic-ultramafic rocks initially formed or emplaced …