Member Since 2005
Julie Prytulak
Professor, Durham University
AGU Research
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Fluids and melt pathway in the Lesser Antilles subduction zone
SUBDUCTION TOP TO BOTTOM (ST2B): THE NATURE OF THE SUBDUCTION INTERFACE, EARTHQUAKES, AND THE ROLES OF FLUIDS VI ORAL
tectonophysics | 15 december 2023
Lidong Bie, Stephen P. Hicks, Andreas Rietbrock, C...
Volatiles are critical ingredient in the dynamics of subduction zones. Despite their significance, the pathways of volatiles and their influences on m...
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The Magmatic Record of Subduction Initiation: An Iron Isotope Perspective
PROCESSES AND IMPACTS OF CRUSTAL RECYCLING: INSIGHTS FROM NONTRADITIONAL STABLE ISOTOPES II ORAL
volcanology, geochemistry and petrology | 15 december 2022
Julie Prytulak, Sophie Page, Kevin W. Burton, Geof...
The average Fe isotopic composition of arc lavas is lighter than mid-ocean ridge basalts. Explanations for the isotopic difference include the degree ...
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Slab to back-arc to arc: fluid and melt pathways through the mantle wedge beneath the Lesser Antilles from seismic attenuation tomography
SUBDUCTION TOP TO BOTTOM (ST2B): ORIGIN AND EVOLUTION OF MAGMATIC ARCS II ORAL
tectonophysics | 12 december 2022
Stephen P. Hicks, Lidong Bie, Catherine Rychert, N...
Volatiles expelled from subducted plates melt the overlying warm mantle, feeding arc volcanism. However, debates remain over the factors controlling m...
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Thallium Isotopic Compositions in Hawaiian Lavas: Evidence for Recycled Materials on the Kea Side of the Hawaiian Mantle Plume
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
02 september 2021
Nicole Williamson, Dominique Weis, Julie Prytulak
Hawaiian volcanoes record 6 Ma of potentially deep mantle chemistry and form two parallel volcanic chains that are geochemically unique, named...
Variation in Upper Plate Crustal and Lithospheric Mantle Structure in the Greater and Lesser Antilles From Ambient Noise Tomography
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
12 july 2021
David Schlaphorst, Nicholas Harmon, J M. Kendall, ...
The crust and upper mantle structure of the Greater and Lesser Antilles Arc provides insights into key subduction zone processes in a unique region...
Magmatic Response to Subduction Initiation, Part II: Boninites and Related Rocks of the Izu‐Bonin Arc From IOPD Expedition 352
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
12 january 2021
John W. Shervais, Mark K. Reagan, Marguerite Godar...
International Ocean Discovery Program Expedition 352 to the Izu‐Bonin forearc cored over 800 m of basement comprising boninite and bonin...
Stable Titanium Isotopic Fractionation During Subduction Initiation of the Izu-Bonin-Mariana Arc
SUBDUCTION INITIATION: MODERN PROCESSES, ANCIENT PRODUCTS, AND NUMERICAL MODELS ELIGHTNING
volcanology, geochemistry and petrology | 16 december 2020
Sophie Page, Julie Prytulak, Marc-Alban Millet, Ge...
Subduction initiation is an enigmatic, yet fundamental process in the plate tectonic cycle. IODP Exp. 352 to the Bonin forearc, recovered the first in...
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Timescales of magma hybridization and remobilization in the steady-state plumbing system of Popocatépetl volcano, Mexico
CONSTRAINING PETROLOGICAL AND GEOCHEMICAL VARIATIONS IN MAGMAS TO CAPTURE THE EVOLUTION OF VOLCANOES OVER SPACE AND TIME: INSIGHTS FROM THE ASIA-PACIFIC, EUROPE/AFRICA, AND AMERICAS REGIONS - SESSION 3
innovative sessions | 15 december 2020
Martin Mangler, Chiara Maria Petrone, Julie Prytul...
Diffusion chronometry is widely used to constrain timescales of pre-eruptive magmatic processes such as ascent rates and mixing-to-eruption timescales...
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