OOIR: Observatory of International Research

Papers

(The H4-Index of Journal of Geophysical Research-Solid Earth is 36. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2022-06-01 to 2026-06-01.)

Article	Citations
Thank You to Our 2023 Reviewers	84
Accuracy of Finite Fault Slip Estimates in Subduction Zone Regions With Topographic Green's Functions and Seafloor Geodesy	81
Issue Information	71
Shear‐Enhanced Electrical Conductivity of Synthetic Quartz‐Graphite Gouges: Implications for Electromagnetic Observations in Carbonaceous Shear Zones	71
Limited Preservation of Strike‐Slip Surface Displacement in the Geomorphic Record	69
The Triggering of Sub‐Plinian and Plinian Eruptions: Insights From Three Decades of InSAR Observations in the Andean Southern Volcanic Zone (1991–2025) and a Global Compilation	67
Hydrogen Concentrations and He Isotopes in Olivine From Ultramafic Lamprophyres Provide New Constraints on a Wet Tarim Plume and Earth's Deep Water Cycle	65
Magmatic Volatile Flux Drives Non‐Eruptive Volcano‐Tectonic Seismicity at Mount St. Helens, USA From 2008–2024	59
Enhancing the Success Rate of Paleointensity Measurements by Integrating Visible and Near‐Infrared Reflectance Spectroscopy and Rock Magnetism	59
Crustal Structure of the J Magnetic Anomaly at 31°N, Northern Central Atlantic	51
Evolution of Stresses Over Conjugate Faults in Hjalli‐Ölfus, South Iceland	50
An Updated Fault Coupling Model Along Major Block‐Bounding Faults on the Eastern and Northeastern Tibetan Plateau From a Stress‐Constrained Inversion of GPS and InSAR Data	50
Insights Into Interfacial Dynamic and Displacement Patterns During Immiscible Two‐Phase Porous Media Flow Under Controlled Viscosity and Wettability Conditions	44
	43
A Limited Effect of Continents on Subduction Initiation for Convection With Grain‐Damage	43
On Dislocation Modeling of Megathrust Tsunami Sources	43
The Matrix Profile in Seismology: Template Matching of Everything With Everything	43
Frictional Contacts Between Rough Grains With Fractal Morphology	43
Evolving Sediment Structure and Lithospheric Architecture Across the Indo‐Burman Forearc Margin From the Joint Inversion of Surface‐ and Scattered‐Wave Seismic Constraints	42
Coupling 3D Geodynamics and Dynamic Rupture: Rheology and Stress Control on Strike‐Slip Fault Evolution and Earthquake Dynamics	42
Lateral Variations in Teleseismic Attenuation of the Conterminous U.S. and New Insights Derived From Its Relationship to Mantle Seismic Velocity	41
A High‐Resolution Shear Velocity Model of the Crust and Uppermost Mantle Beneath Westernmost Mediterranean Including Radial Anisotropy	41
Inherited Lithospheric Structure Controls Cenozoic Intraplate Basaltic Volcanism in Central Mongolia Due To Mantle Upwelling	41
Characteristics of the Matuyama‐Brunhes Magnetic Field Reversal Based on a Global Data Compilation	40
Passive Sources and Diffracted Points Imaging Using Combinational Cross‐Correlation Imaging Condition	39

Seismic Observation of a New ULVZ Beneath the Southern Pacific	39
Bathymetric Prediction Using Multisource Gravity Data Derived From a Parallel Linked BP Neural Network	39
Mechanisms for Layered Anisotropy and Anomalous Magmatism of Alaska Subduction System Revealed by Ambient Noise Tomography and the Wave Gradiometry Method	39
Manganese Cycling Driven by Fluctuating Redox Chemocline in the Ediacaran Ocean	38
On the Constitutive Equations for Coupled Flow, Chemical Reaction, and Deformation of Porous Media	38
Automatic Detection of InSAR Deformation and Tropospheric Noise Features Using Computer Vision: A Case Study Over West Texas	37
Cluster Analysis of Dense GNSS Velocity Field Reveals Characteristics Associated With Regional Tectonics in New Zealand	37
The Evolution of Fault Networks During Multiphase Triaxial and Biaxial Strain: An Analogue Modeling Approach	36
Formation of Thermochemical Heterogeneities by Core‐Mantle Interaction	36
Gradually Hydrating Upper Mantle and a Moderately Wet Mantle Transition Zone Determined From Wadsleyite‐Olivine Phase Relations	36
Theoretical Modeling of Secondary Microseisms Considering Source and Receiver Site Structures, With a Focus on Ocean‐Bottom Sediment Effects	36