Subduction-driven volatile recycling: A global mass balance
Volatile elements (water, carbon, nitrogen, sulfur, halogens, and noble gases) played an
essential role in the secular evolution of the solid Earth and emergence of life. Here we …
essential role in the secular evolution of the solid Earth and emergence of life. Here we …
Magmatic volatiles (H, C, N, F, S, Cl) in the lunar mantle, crust, and regolith: Abundances, distributions, processes, and reservoirs
FM McCubbin, KEV Kaaden, R Tartèse… - American …, 2015 - degruyter.com
Many studies exist on magmatic volatiles (H, C, N, F, S, Cl) in and on the Moon, within the
last several years, that have cast into question the post-Apollo view of lunar formation, the …
last several years, that have cast into question the post-Apollo view of lunar formation, the …
Recurring volcanic winters during the latest Cretaceous: Sulfur and fluorine budgets of Deccan Traps lavas
Two events share the stage as main drivers of the Cretaceous-Paleogene mass extinction—
Deccan Traps volcanism, and an asteroid impact recorded by the Chicxulub crater. We …
Deccan Traps volcanism, and an asteroid impact recorded by the Chicxulub crater. We …
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 …
The lunar apatite paradox
JW Boyce, SM Tomlinson, FM McCubbin… - Science, 2014 - science.org
Recent discoveries of water-rich lunar apatite are more consistent with the hydrous magmas
of Earth than the otherwise volatile-depleted rocks of the Moon. Paradoxically, this requires …
of Earth than the otherwise volatile-depleted rocks of the Moon. Paradoxically, this requires …
Experimental melting of phlogopite-peridotite in the garnet stability field
Melting experiments have been performed at 3 GPa, between 1150 and 1450° C, on a
phlogopite-peridotite source in the garnet stability field. We succeeded to extract and …
phlogopite-peridotite source in the garnet stability field. We succeeded to extract and …
Two-component mantle melting-mixing model for the generation of mid-ocean ridge basalts: Implications for the volatile content of the Pacific upper mantle
We report major, trace, and volatile element (CO 2, H 2 O, F, Cl, S) contents and Sr, Nd, and
Pb isotopes of mid-ocean ridge basalt (MORB) glasses from the Northern East Pacific Rise …
Pb isotopes of mid-ocean ridge basalt (MORB) glasses from the Northern East Pacific Rise …
The evolution of the lunar crust
1609 AD marked the beginning of the modern scientific exploration of the Moon's crust when
Thomas Harriot and later Galileo Galilei made the first recorded maps of the nearside with …
Thomas Harriot and later Galileo Galilei made the first recorded maps of the nearside with …
Halogen geochemistry of I-and A-type granites from Jiuhuashan region (South China): Insights into the elevated fluorine in A-type granite
Spatially associated A-and I-type granites and mafic dyke rocks from the Jiuhuashan region
(South China) have been geochemically studied with a special emphasis on their halogen …
(South China) have been geochemically studied with a special emphasis on their halogen …
Pyroxenes as tracers of mantle water variations
JM Warren, EH Hauri - Journal of Geophysical Research: Solid …, 2014 - Wiley Online Library
The concentration and distribution of volatiles in the Earth's mantle influence properties such
as melting temperature, conductivity, and viscosity. To constrain upper mantle water content …
as melting temperature, conductivity, and viscosity. To constrain upper mantle water content …