Chris Marone
flowchart A[Chris Marone] AC["Associated Concepts (21)"] AW["Authored Works (17)"] CA["Linked Co-Authors (27)"] CI["Linked Collaborating Institutions (13)"] A== dcterms:relation ==>AC AW== author ==>A AW== author ==>CA AW== affil ==>CI click AC "#associated-concepts" click AW "#authored-works" click CA "#co-authors" click CI "#collaborating-institutions" NI["add incoming edge"] NO["add outgoing edge"] NI-- ? -->A A-- ? -->NO click NI "#add-incoming-edge" click NO "#add-outgoing-edge" style NI stroke-width:2px,stroke-dasharray: 5 5 style NO stroke-width:2px,stroke-dasharray: 5 5
- ORCiD
- https://orcid.org/0000-0002-4515-4500
- OpenAlex ID
- https://openalex.org/A5069588793 (API record)
Associated Concepts [?]
- Geology
- Engineering
- Physics
- Biology
- Paleontology
- Materials science
- Thermodynamics
- Composite material
- Seismology
- Geotechnical engineering
- Aerospace engineering
- Slip (aerodynamics)
- Fault (geology)
- Chemistry
- Quantum mechanics
- Petrology
- Mechanics
- Shear (geology)
- Metallurgy
- Fault gouge
- Computer science
Authored Works
sorted by decreasing year, and then by display-name
- The effect of normal stress oscillations on the slip behavior of a critically stable fault
- The Role of Pore Fluids on Fault Stability at Drained Boundary Conditions
- Nucleation processes and foreshocks of slow and fast laboratory earthquakes illuminated with waveform similarity measurements
- Laboratory earthquake forecasting using elastic wave properties and machine learning
- Illuminating Fundamental Processes Governing Evolution of Fault Zone Permeability and Elastodynamic Properties due to Dynamic Stressing using a Coupled X-Ray Imaging and Active Ultrasonic Experiment
- Frictional Healing of Ancient Subduction-related Mélanges- the Role of Pressure Solution
- Decoupling the poromechanics of particle remobilization and interface stiffness of dynamically stressed tensile fractured rock
- An Integrated Experimental and Multi-Physics Numerical Study on the Interplay Between Hydraulic and Elastic Properties of Fractured Rock Interfaces Under Stress Perturbations
- Acoustic signature of fault slip from slow to fast earthquake: a laboratory insight
- A Physics-informed Machine Learning (PIML) Model for Lab Earthquake Prediction using Time-lapse Active Source Ultrasonic Data
- The Role of Element Transport in Subduction Fault Zone Restrengthening
- Relating Fracture Aperture to Hydraulic and Elastodynamic Properties of Dynamically-stressed Under True-triaxial Stress Conditions
- Modulating Fault Instability with Pore Fluid Pressures
- Identification and Observations of Dynamically Triggered Earthquakes near the Alto Tiberina Fault in the central Apennines, Italy
- Frictional and Lithological Controls on Shallow Slow Slip at the Northern Hikurangi Margin
- Creep fronts and asperity interactions in laboratory earthquake sequences illuminate delayed earthquake triggering
- Bifurcations at the Stability Transition of Earthquake Faulting
Linked Co-Authors
- A. A. Hutchison
- Alessandro Vuan
- Andrew J. Smye
- Carolina Giorgetti
- Chun‐Yu Ke
- Clay Wood
- Corentin Noël
- Cristiano Collettini
- D. M. Saffer
- Daniel T. Trugman
- David S. Kammer
- Deepa Mele Veedu
- Donald M. Fisher
- Elisa Tinti
- Federico Pignalberi
- Gregory C. McLaskey
- Jacques Rivière
- L. Chiaraluce
- M. M. Scuderi
- Matt J. Ikari
- Parisa Shokouhi
- Raphael Affinito
- S. B. L. Cebry
- Samson Marty
- Srisharan Shreedharan
- Sylvain Barbot
- Y. Hashimoto
Linked Collaborating Institutions
- Cornell University, New York
- Eidgenossische Technische Hochschule, Zurich, Switzerland
- Kochi University, Japan
- Nanyang Technological University, Singapore
- National Institute for Oceanography and Experimental Geophysics, Italy
- National Institute of Geophysics and Volcanology, Italy
- Pennsylvania State University
- Sapienza University, Rome, Italy
- University of Bremen, Center for Marine Environmental Sciences
- University of South Florida
- University of Southern California
- University of Texas, Austin
- University of Texas, Austin, Department of Geological Sciences
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