John W. Shervais

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Professor

Utah State University

United States

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John W. Shervais is a Professor at Utah State University in the United States. His research focuses on geosciences, with recent publications addressing topics such as metasomatism and melting processes in lithospheric substrates, geological analysis of submarine basalt flows, and geothermal play fairway methodologies. He has contributed significantly to the understanding of magmatic processes and structural inheritance in various geological settings.

Recent Grants

Grant: Close

Collaborative Research: Subduction Initiation and Development of the nascent Izu-Bonin-Mariana arc

Open Date: 2016-06-01

Close Date: 2018-05-01

Grant: Close

Phase 2: Play Fairway Analysis of the Snake River Plain, Idaho

Open Date: 2016-02-01

Close Date: 2017-09-01

Grant: Close

Post Expedition Award - IODP Expedition 352

Open Date: 2014-11-01

Close Date: 2016-03-01

Grant: Close

Play Fairway Analysis of the Snake River Plain, Idaho: Phase 1

Open Date: 2014-10-01

Close Date: 2016-02-01

Grant: Close

Salary Support for John Shervais - IODP Expedition 352

Open Date: 2014-07-01

Close Date: 2015-03-01

Articles (17)

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2020

Collaborators (14)

James Evans

Professor

Utah State University

UNITED STATES

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Australian National University

AUSTRALIA

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Mark Reagan

Professor

Iowa State University

UNITED STATES

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Julie Prytulak

University of Durham

UNITED KINGDOM

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John W. Shervais

Research Interests

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Recent Grants

Articles (17)

Eruption, Emplacement and Internal Architecture of Massive and Super‐Massive Inflated Submarine Basalt Lava Flows, Walvis Ridge Hotspot Track, IODP Expeditions 391/397T

Metasomatism and Melting of Cordilleran Lithosphere Resulting From Sediment Relamination During Shallow Subduction

Structural inheritance in Carolinia, external to the excised Rheic suture: Savannah River Site, South Carolina, U.S.A.

Geothermal play fairway analysis, part 1: Example from the Snake River Plain, Idaho

Preliminary Characterization of Submarine Basalt Magnetic Mineralogy Using Amplitude‐Dependence of Magnetic Susceptibility

Timescales of mafic magmatic fractionation documented by paleosecular variation in basaltic drill core, Snake River Plain volcanic province, Idaho, USA

Geothermal Play Fairway Analysis, Part 2: GIS methodology

Re−Os Isotope and PGE Abundance Systematics of Coast Range Ophiolite Peridotites and Chromitite, California: Insights into Fore-Arc Magmatic Processes

Expedition 391 methods

Expedition 391 summary

Petrologic evolution of boninite lavas from the IBM Fore-Arc, IODP Expedition 352: Evidence for open-system processes during early subduction zone magmatism

Shallow Depth, Substantial Change: Fluid-Metasomatism Causes Major Compositional Modifications of Subducted Volcanics (Mariana Forearc)

The petrogenesis of modern and ophiolitic lavas reconsidered: Ti-V and Nb-Th

Magma Source Evolution Following Subduction Initiation: Evidence From the Element Concentrations, Stable Isotope Ratios, and Water Contents of Volcanic Glasses From the Bonin Forearc (IODP Expedition 352)

Magmatic Response to Subduction Initiation, Part II: Boninites and Related Rocks of the Izu‐Bonin Arc From IODP Expedition 352

Mineral compositions and thermobarometry of basalts and boninites recovered during IODP Expedition 352 to the Bonin forearc

Mariana serpentinite mud volcanism exhumes subducted seamount materials: Implications for the origin of life

Collaborators (14)

James Evans

Baptiste Debret

Timothy Chapman

Jesse Scholpp

Dennis Newell

Lee Liberty

Jeffrey Ryan

Catriona Menzies

William Sager

Zachary Atlas

Wendy R. Nelson

Yuhao Dai

Mark Reagan

Julie Prytulak

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