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Earth's mantle

Structure of hydrous eutectic silicate melts at different temperatures and pressures
Posted inEditors' Highlights

Hiding Deep Hydrous Melts at the Core-Mantle Boundary

by S. D. Jacobsen 13 September 20194 August 2023

Silicate melts containing H2O in the lowermost mantle are surprisingly dense and may stagnate there, trapping primordial volatiles and potentially causing some of the ultra-low velocity zones.

Graph showing the possible melting curve of hydrogen-bearing iron peroxide
Posted inEditors' Highlights

The Lower Mantle May Have a Wet Bottom

by S. W. Parman 6 August 20194 August 2023

Molecular dynamics calculations suggest that molten hydrogen-bearing iron peroxide (FeO2Hx) may produce the ultra-low velocity zones that occur at the core-mantle boundary.

Posted inEditors' Highlights

Seismic Anisotropy Due to a Compositionally Layered Mantle

by Bjarne S. G. Almqvist 8 March 20198 July 2024

Investigating the role of layered rocks and compositional banding on mineral scale in generating seismic anisotropy in the mantle.

Posted inEditors' Highlights

Carbonate Melting Enhances Mantle CO2 Fluxes in Old Ocean Basins

by S. D. Jacobsen 17 August 20184 August 2023

The amount of CO2 segregated from the mantle by carbonate melting beneath old oceanic crust may equal that emitted along the mid-ocean ridge system, thereby contributing to the global carbon cycle.

New evidence suggests volcanoes on China’s Hainan Island are the result of a hot spot
Posted inResearch Spotlights

Linking Mantle Plumes to Volcanoes and Hot Spot Tracks

by E. Underwood 11 June 20184 August 2023

Study bolsters hypothesis that volcanoes on China’s Hainan Island were formed by a hot spot.

A rough, uncut diamond sitting in kimberlite rock.
Posted inNews

Diamond Impurities Reveal Water Deep Within the Mantle

Kimberly M. S. Cartier, News Writing and Production Intern for Eos.org by Kimberly M. S. Cartier 2 April 20184 August 2023

A high-pressure form of ice, trapped within diamonds forged in the lower mantle, suggests that aqueous fluids reside deeper in Earth than we knew.

Researchers examine how mantle upwelling under oceanic transform faults stabilizes these boundaries.
Posted inResearch Spotlights

Widespread Mantle Upwelling Beneath Oceanic Transform Faults

by Terri Cook 13 March 20188 July 2024

A global characterization of mantle flow patterns beneath active oceanic transforms suggests pervasive upwelling stabilizes divergent plate boundaries by warming and weakening these enigmatic features.

Posted inEditors' Highlights

New Thermodynamic Model for Computing Mantle Mineralogy

by M. Walter 16 January 20184 August 2023

A newly developed open-access software package called MMA-EoS can calculate whole mantle mineralogy in multicomponent systems by Gibbs energy minimization.

Studying volcanic eruptions in Iceland lends insight into the mantle temperature below.
Posted inResearch Spotlights

A Significantly Hotter Mantle Beneath Iceland

by Terri Cook 18 November 20164 August 2023

Estimates of crystallization temperatures from four eruptions in northern Iceland offer improved constraints on the mantle's temperature beneath this anomalous divergent plate boundary.

research-model-temperature-mantle-melting-pyroxenites
Posted inResearch Spotlights

A Better Model for How the Mantle Melts

Kate Wheeling, freelance science writer by Kate Wheeling 28 September 20164 August 2023

A new model of the melting behavior of certain mantle rocks gives researchers a better understanding of the source of oceanic lavas.

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