John Naliboff

Assistant Professor

New Mexico Institute of Mining and Technology

United States

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About

John Naliboff is an Assistant Professor at the New Mexico Institute of Mining and Technology in the United States. His research focuses on solid dynamics, interface rheology, and slab hydration, with recent articles exploring the Hikurangi Subduction Zone and Hawaiian lithosphere dynamics. He also investigates rift-inversion orogens, crustal strength influences on rift geometry, and the interactions between plume and lithosphere beneath the East African Rift.

Articles (10)

Year:

2025

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2025

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2025

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2025

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2023

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2023

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2023

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2023

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2023

Year:

2022

Collaborators (8)

Jeroen van Hunen

Professor

University of Durham

UNITED KINGDOM

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Timo Heister

Clemson University

UNITED STATES

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D. Sarah Stamps

Associate Professor

Virginia Tech

UNITED STATES

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Dylan Vasey

Assistant Professor

Tufts University

UNITED STATES

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Sascha Brune

Professor

University of Potsdam

GERMANY

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Kenneth McCaffrey

Professor

University of Durham

UNITED KINGDOM

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Magali Billen

Professor

University of California, Davis

UNITED STATES

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Clinton Conrad

Professor

University of Oslo

NORWAY

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John Naliboff

Research Interests

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About

Articles (10)

Using Subducting Plate Motion to Constrain Cascadia Slab Geometry and Interface Strength

Rift-inversion orogens are potential hotspots for natural H2 generation

Constraining Solid Dynamics, Interface Rheology, and Slab Hydration in the Hikurangi Subduction Zone Using 3‐Dimensional Fully Dynamic Models

Magma‐Assisted Flexure of Hawaiian Lithosphere Inferred From Three‐Dimensional Models of Lithospheric Flexure Constrained by Active Source Seismic Data

Modeling Viscoelastic Solid Earth Deformation Due To Ice Age and Contemporary Glacial Mass Changes in ASPECT

A Geodynamic Investigation of Plume‐Lithosphere Interactions Beneath the East African Rift

The influence of crustal strength on rift geometry and development – insights from 3D numerical modelling

How Do Rift‐Related Fault Network Distributions Evolve? Quantitative Comparisons Between Natural Fault Observations and 3D Numerical Models of Continental Extension

Utilization of continental transforms in break-up: observations, models, and a potential link to magmatism

Solid Earth Uplift Due To Contemporary Ice Melt Above Low‐Viscosity Regions of the Upper Mantle

Collaborators (8)

Jeroen van Hunen

Timo Heister

D. Sarah Stamps

Dylan Vasey

Sascha Brune

Kenneth McCaffrey

Magali Billen

Clinton Conrad

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