TG
Member Since 1973
Tim L. Grove
Professor, Geology, Massachusetts Institute of Technology
AGU Research
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Garnet Lherzolite as the Source of Tholeiitic Melts in Kamaʻehuakanaloa
CHEMISTRY AND EVOLUTION OF EARTH’S INTERIOR AS RECORDED BY MANTLE PLUMES I POSTER
volcanology, geochemistry and petrology | 13 december 2023
Susana Hoyos, Stephanie M. Krein, Timothy L. Grove
The mantle source composition of low-silica, TiO2-rich Hawaiian tholeiitic lavas is an ongoing debate between two contrasting models: a pyroxenite sou...
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Plagioclase Lherzolite Melting: Experimental Constraints on a Primary, High‐Alumina MORB From the Southwest Indian Ridge
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
26 october 2023
Patrick Beaudry, Stephanie M. Krein, Timothy L. Gr...

We experimentally investigated the phase relations of a primary basaltic glass erupted on the 10–15°E ultraslow spreading (∼0.4...

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Differentiation of the Angrite Parent Body: implications of a moon-sized planetesimal in the early Solar System.
ACCRETION AND DIFFERENTIATION OF ROCKY PLANETS FROM INTERDISCIPLINARY PERSPECTIVES I ORAL
study of earth's deep interior | 14 december 2022
Susana Hoyos, Timothy L. Grove
Angrites are a group of basaltic achondrites formed in a differentiated body that began accreting in the first 4 Myr of the Solar System. They record ...
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Multiple Sulfur Isotope Insights on the Tectonic Evolution of the 4.02–2.94 Ga Acasta Gneiss Complex
FROM THE SURFACE TO THE DEEP INTERIOR OF THE EARLY EARTH II POSTER
study of earth's deep interior | 12 december 2022
Patrick Beaudry, Ann Bauer, Jesse R. Reimink, Gare...
The Acasta Gneiss Complex (AGC) of the Canadian Northwest Territories represents the oldest known evolved crust, with zircon UPb ages up to 4.03 Ga. C...
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Temperatures and Timescales of Crystallization in the “Mush Zone” Beneath Fast‐Spreading Ocean Ridges
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
01 december 2022
Jill A. VanTongeren, Peter B. Kelemen, Timothy L. ...

Quantifying the timescales of magma solidification and eruption beneath mid‐ocean ridges is critical to understanding how melts are emplaced ...

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Petrologic constraints on the occurrence of garnet-lherzolite melts in the mantle source under Loihi, Hawaii
THE MAGMATIC PLUMBING SYSTEMS OF OCEANIC ISLANDS I ORAL
volcanology, geochemistry and petrology | 16 december 2021
Susana Hoyos, Stephanie M. Krein, Timothy L. Grove
Tholeiitic glasses from Loihi seamount, the youngest volcano in the Hawaiian-Emperor chain, are thought to represent decompression melts of garnet-lhe...
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An experimental approach for studying sulfur in high pressure, oxidized and hydrous melts
CONNECTING THE DEEP AND SURFICIAL DOTS: LINKING PETROLOGY AND GAS MEASUREMENTS TO CONSTRAIN VOLATILE BEHAVIOR IN VOLCANIC SYSTEMS I ORAL
volcanology, geochemistry and petrology | 16 december 2021
Patrick Beaudry, Timothy L. Grove
Understanding the mechanisms by which sulfur is transported from the mantle to the surface in volcanic-geothermal environments is critical for interpr...
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Global Mid-Ocean Ridge Melting Conditions Constrained from 13,589 Basaltic Glasses
FOCUSED OBSERVATIONS OF RIDGE NEAR-AXIS REMOTE AND IN SITU INVESTIGATIONS: MAGMATIC, VOLCANIC, HYDROTHERMAL, AND BIOLOGICAL PROCESSES II ORAL
volcanology, geochemistry and petrology | 15 december 2021
Stephanie M. Krein, Zachary Molitor, Timothy L. Gr...
We have developed a model, ReversePetrogen (RevPet), to predict mantle melting conditions (pressure, temperature, source composition) using erupted ba...
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