John Naliboff
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View article: Fatbox: the fault analysis toolbox
Fatbox: the fault analysis toolbox Open
Understanding complex fault networks is essential for reconstructing their geological history, quantifying deformation in tectonically active regions, and assessing geohazards and resource potentials. Structure and evolution of fault netwo…
View article: Technical note: Geodynamic Thermochronology (GDTchron) – A Python package to calculate low-temperature thermochronometric ages from geodynamic numerical models
Technical note: Geodynamic Thermochronology (GDTchron) – A Python package to calculate low-temperature thermochronometric ages from geodynamic numerical models Open
Low-temperature thermochronology provides a powerful means of extracting quantitative information on the thermal evolution of different tectonic settings from rocks exposed at the surface of the Earth. Geodynamic numerical models enable tr…
View article: Magma‐Assisted Flexure of Hawaiian Lithosphere Inferred From Three‐Dimensional Models of Lithospheric Flexure Constrained by Active Source Seismic Data
Magma‐Assisted Flexure of Hawaiian Lithosphere Inferred From Three‐Dimensional Models of Lithospheric Flexure Constrained by Active Source Seismic Data Open
Reprocessed and newly acquired seismic data provide new constraints on lithospheric flexure profiles beneath the Hawaiian Islands. We use these new observations and three‐dimensional numerical models of lithospheric deformation combining e…
View article: Constraining Solid Dynamics, Interface Rheology, and Slab Hydration in the Hikurangi Subduction Zone Using 3‐Dimensional Fully Dynamic Models
Constraining Solid Dynamics, Interface Rheology, and Slab Hydration in the Hikurangi Subduction Zone Using 3‐Dimensional Fully Dynamic Models Open
Simulating present‐day solid Earth deformation and volatile cycling requires integrating diverse geophysical data sets and advanced numerical techniques to model complex multiphysics processes at high resolutions. Subduction zone modeling …
View article: Using Subducting Plate Motion to Constrain Cascadia Slab Geometry and Interface Strength
Using Subducting Plate Motion to Constrain Cascadia Slab Geometry and Interface Strength Open
Subduction zones are home to multiple geohazards driven by the evolution of the regional tectonics, including earthquakes, volcanic eruptions and landslides. Past evolution builds the present‐day structure of the margin, while the present‐…
View article: Rift-inversion orogens are potential hot spots for natural H <sub>2</sub> generation
Rift-inversion orogens are potential hot spots for natural H <sub>2</sub> generation Open
Naturally occurring hydrogen gas (H 2 ) represents a potential source of clean energy. A promising mechanism for large-scale natural H 2 generation is serpentinization of exhumed mantle material. We study this serpentinization-related H 2 …
View article: Evaluating Segmentation Behavior Along the Alamogordo Fault, central New Mexico, Using Neotectonic Mapping, Soil Chronosequences, and Geodynamic Modeling
Evaluating Segmentation Behavior Along the Alamogordo Fault, central New Mexico, Using Neotectonic Mapping, Soil Chronosequences, and Geodynamic Modeling Open
Earthquake magnitude scales with the length of the ruptured fault plane.Regional seismic hazard assessments therefore require an understanding of how individual fault segments may link together to produce large earthquakes.Though fault seg…
View article: Exploring the structure of the Cascadia Subduction Zone by coupling 3D thermomechanical modeling and CPO evolution with observations.
Exploring the structure of the Cascadia Subduction Zone by coupling 3D thermomechanical modeling and CPO evolution with observations. Open
The Cascadia Subduction Zone is characterized by young subducting lithosphere, its isolation from other subducting systems, and its ability to produce megathrust earthquakes (M>9.0) and devastating tsunamis. Due to its high potential hazar…
View article: Rift-inversion orogens are the place to be for natural hydrogen gas (H2) exploration
Rift-inversion orogens are the place to be for natural hydrogen gas (H2) exploration Open
Naturally occurring hydrogen gas (H2) represents a potentially major source of clean energy. It has been relatively overlooked so far but has gained more attention recently. The most promising mechanism for large-scale generation of such n…
View article: Impact of rift history on the structural style of intracontinental rift-inversion orogens
Impact of rift history on the structural style of intracontinental rift-inversion orogens Open
Although many collisional orogens form after subduction of oceanic lithosphere between two continents, some orogens result from strain localization within a continent via inversion of structures inherited from continental rifting. Intracon…
View article: Rift-inversion orogens are potential hotspots for natural H2 generation
Rift-inversion orogens are potential hotspots for natural H2 generation Open
Naturally occurring hydrogen gas (H2) represents a potentially major source of clean energy. The most promising mechanism for large-scale natural H2 generation is serpentinization where mantle material reacts with water while passing throu…
View article: How Do Rift‐Related Fault Network Distributions Evolve? Quantitative Comparisons Between Natural Fault Observations and 3D Numerical Models of Continental Extension
How Do Rift‐Related Fault Network Distributions Evolve? Quantitative Comparisons Between Natural Fault Observations and 3D Numerical Models of Continental Extension Open
Continental extension is primarily accommodated by the evolution of normal fault networks. Rifts are shaped by complex tectonic processes and it has historically been difficult to determine the key rift controls using only observations fro…
View article: Impact of rift history on the structural style of intracontinental rift-inversion orogens
Impact of rift history on the structural style of intracontinental rift-inversion orogens Open
Although many collisional orogens form after subduction of oceanic lithosphere between two continents, some orogens result from strain localization within a continent via inversion of structures inherited from continental rifting. Intracon…
View article: Evaluating Segmentation Behavior Along the Alamogordo Fault Using Remote Sensing and Field-based Datasets
Evaluating Segmentation Behavior Along the Alamogordo Fault Using Remote Sensing and Field-based Datasets Open
Earthquake magnitude scales with the length of the ruptured fault plane (Wells and Coppersmith, 1994).Regional earthquake hazard assessments therefore require an understanding of how individual fault segments may link together to produce l…
View article: The influence of crustal strength on rift geometry and development – insights from 3D numerical modelling
The influence of crustal strength on rift geometry and development – insights from 3D numerical modelling Open
The lateral distribution of strength within the crust is non-uniform, dictated by crustal lithology and the presence and distribution of heterogeneities within it. During continental extension, areas of crust with distinct lithological and…
View article: Modeling Viscoelastic Solid Earth Deformation Due To Ice Age and Contemporary Glacial Mass Changes in ASPECT
Modeling Viscoelastic Solid Earth Deformation Due To Ice Age and Contemporary Glacial Mass Changes in ASPECT Open
The redistribution of past and present ice and ocean loading on Earth's surface causes solid Earth deformation and geoid changes, known as glacial isostatic adjustment. The deformation is controlled by elastic and viscous material paramete…
View article: Normal fault network evolution in 3D numerical models
Normal fault network evolution in 3D numerical models Open
Understanding how normal fault networks initiate and evolve is important for quantifying plate boundary deformation, assessing seismic hazard and finding natural resources. In recent years, 3D numerical models have been developed that can …
View article: Numerical modelling of mantle exhumation in inverted rift systems
Numerical modelling of mantle exhumation in inverted rift systems Open
The tectonic exhumation of mantle material is a well-known phenomenon and may occur during both rifting and subsequent (large-scale) basin inversion. However, the processes leading to the exhumation of dense and therefore negatively buoyan…
View article: [DATASET] How do rift-related fault network distributions evolve?
[DATASET] How do rift-related fault network distributions evolve? Open
Here we provide the Supplementary Material for the publication 'How do rift-related fault network distributions evolve? Quantitative comparisons between natural fault observations and 3D numerical models of continental extension'…
View article: The influence of crustal strength on rift geometry and development – Insights from 3D numerical modelling
The influence of crustal strength on rift geometry and development – Insights from 3D numerical modelling Open
The lateral distribution of strength within the crust is non-uniform, dictated by crustal lithology and the presence and distribution of heterogeneities within it. During continental extension, areas of crust with distinct lithological and…
View article: The influence of crustal strength on rift geometry and development –Insights from 3D numerical modelling
The influence of crustal strength on rift geometry and development –Insights from 3D numerical modelling Open
Data, software, and animations related to the publication "The influence of crustal strength on rift geometry and development –Insights from 3D numerical modelling", submitted by Phillips et al. to Solid Earth. A preprint of this article i…
View article: Kinematic and rheological controls on rift-related fault evolution
Kinematic and rheological controls on rift-related fault evolution Open
Continental extension is primarily accommodated by the evolution of normal fault networks. Rifts are shaped by complex tectonic processes and it has historically been difficult to determine the key rift controls using only observations fro…
View article: Solid Earth Uplift Due To Contemporary Ice Melt Above Low‐Viscosity Regions of the Upper Mantle
Solid Earth Uplift Due To Contemporary Ice Melt Above Low‐Viscosity Regions of the Upper Mantle Open
Glacial isostatic adjustment explains topographic change in formerly and currently glaciated regions, but the role of small (∼100s km) regions of unusually low‐viscosity mantle is poorly understood. We developed viscoelastic models with lo…
View article: Bridging Spatiotemporal Scales of Normal Fault Growth During Continental Extension Using High‐Resolution 3D Numerical Models
Bridging Spatiotemporal Scales of Normal Fault Growth During Continental Extension Using High‐Resolution 3D Numerical Models Open
Continental extension is accommodated by the development of kilometer‐scale normal faults, which grow during meter‐scale slip events that occur over millions of years. However, reconstructing the entire lifespan of a fault remains challeng…
View article: Modelling ridge jumps in back-arc basins at different scales
Modelling ridge jumps in back-arc basins at different scales Open
<p>The structure of oceanic back-arc basins reflects the dynamics of the subduction zone they are associated with. Often, the basement of these basins is not only composed of oceanic crust, but also of exhumed mantle, fragments of co…
View article: Exploring the Cascadia slab structure coupling 3D thermomechinal and CPO modeling.
Exploring the Cascadia slab structure coupling 3D thermomechinal and CPO modeling. Open
<p>The Cascadia Subduction Zone is characterized by young subducting lithosphere, its isolation from other subducting slabs, and its ability to produce megathrust earthquakes (M>9.0) and devastating tsunamis. Due to its high poten…
View article: The effect of inheritance, rheology, and stress orientation on the 4-D evolution of rift systems
The effect of inheritance, rheology, and stress orientation on the 4-D evolution of rift systems Open
<p>Continental rifts often show a complex spatial and temporal evolution, controlled by the intricate interaction of several ingredients. Inheritance, plate rheology, and stress orientation are amongst the main factors that shape rif…
View article: Life and Death of Normal Faults:&#160;Quantitative Analysis of Fault Network Evolution in 3D Rift Models
Life and Death of Normal Faults: Quantitative Analysis of Fault Network Evolution in 3D Rift Models Open
<p>Quantifying the spatial and temporal evolution of fault systems is crucial in understanding plate boundary deformation and the associated seismic hazard, as well as to help georesources exploration in sedimentary basins. During th…
View article: Continental Rifting Advances Using 3D Computational Modeling of Lithospheric Deformation, Asthenospheric Flow, and Deep Melt Generation with ASPECT&#160;
Continental Rifting Advances Using 3D Computational Modeling of Lithospheric Deformation, Asthenospheric Flow, and Deep Melt Generation with ASPECT  Open
<p>Continental rifting processes are influenced by viscous coupling of the deforming lithosphere to asthenospheric flow, as well as magma that migrates upward from the upper asthenosphere. Over the past few decades, significant advan…
View article: Bridging spatiotemporal scales of normal fault growth during continental extension using high-resolution 3D numerical models: DATASET
Bridging spatiotemporal scales of normal fault growth during continental extension using high-resolution 3D numerical models: DATASET Open
This dataset supplements the publication “Bridging spatiotemporal scales of normal fault growth during continental extension using high-resolution 3D numerical models“ by Pan, Naliboff, Bell and Jackson in Geo…