E
Eric Mittelstaedt
Researcher at University of Idaho
Publications - 39
Citations - 858
Eric Mittelstaedt is an academic researcher from University of Idaho. The author has contributed to research in topics: Lithosphere & Ridge. The author has an hindex of 14, co-authored 38 publications receiving 733 citations. Previous affiliations of Eric Mittelstaedt include Woods Hole Oceanographic Institution & Pierre-and-Marie-Curie University.
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Mid-ocean ridge jumps associated with hotspot magmatism
TL;DR: In this article, the authors used the hybrid finite-element code (FLAC) to simulate viscous mantle flow, elasto-plastic deformation of the lithosphere and heat transport in a ridge setting near an off-axis hotspot.
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Magmatic and tectonic evolution of the North Atlantic
TL;DR: In this article, the authors review the tectonomagmatic evolution of the North Atlantic and constrain evolutionary models with new lithosphere strength estimates and interpretation of potential field data north of Iceland.
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Rheological and mechanical properties of silica colloids: from Newtonian liquid to brittle behaviour
TL;DR: In this article, the authors investigated the properties of aqueous mono-disperse silica suspensions (Ludox® HS40) as a function of particle volume fraction and water content, using shear rate tests, oscillatory methods, indentation and an ultrasonic technique.
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Structure, temporal evolution, and heat flux estimates from the Lucky Strike deep‐sea hydrothermal field derived from seafloor image mosaics
Thibaut Barreyre,Javier Escartín,Rafael Garcia,Mathilde Cannat,Eric Mittelstaedt,Ricard Prados +5 more
TL;DR: In this paper, a study of the Lucky Strike hydrothermal field is presented, showing that repeated image surveys can be performed to characterize and study the temporal variability of a broad range of vent sites hosting active processes.
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Repeat ridge jumps associated with plume‐ridge interaction, melt transport, and ridge migration
TL;DR: In this article, the authors use numerical models to simulate viscous flow of the mantle, viscoplastic deformation of the lithosphere, and melt migration upward from the asthenospheric melting zone, laterally along the base of the upper mantle, and vertically through the upper lithosphere.