LOUIS DE BARROS

Assistant professor

Université de Nice Sophia Antipolis

France

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Louis De Barros is an Assistant Professor at Université de Nice Sophia Antipolis in France. His research primarily focuses on the dynamics of seismic activity, particularly the interactions between fluids and seismic events. Recent articles explore topics such as foreshock identification, slow slip phenomena, and seismic monitoring capabilities, contributing valuable insights into earthquake swarm mechanics.

Articles (16)

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2025

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2024

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2024

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2024

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2023

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2023

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2022

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2022

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2022

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2022

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2021

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2021

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2021

Collaborators (4)

Frantisek Gallovic

Professor

Charles University

CZECH REPUBLIC

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Frédéric Cappa

Professor of Geophysics

Université Côte d'Azur

FRANCE

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Philippe Charvis

Institut de Recherche pour le Développement

FRANCE

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Nicholas Voulgaris

GREECE

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LOUIS DE BARROS

Research Interests

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Articles (16)

Does Foreshock Identification Depend on Seismic Monitoring Capability?

Systematic observation of a seismic back-front during fluid injection in both natural and anthropogenic earthquake swarms

Control of Seismicity Migration in Earthquake Swarms by Injected Fluid Volume and Aseismic Crack Propagation

Parallel dynamics of slow slips and fluid-induced seismic swarms

Induced microseismicity and tremor signatures illuminate different slip behaviours in a natural shale fault reactivated by a fluid pressure stimulation (Mont Terri)

Swarms and mainshock–aftershocks sequences are both triggered by fluids in the Ubaye Region (Western Alps)

Spatio‐Temporal Evolution of Aftershock and Repeater Source Properties After the 2016 Pedernales Earthquake (Ecuador)

The 2020–2021 seismic sequence in the Western Gulf of Corinth: Insights on the triggering mechanisms through high resolution seismological and geodetic data analysis

Inferring fluid volume during earthquake swarms using seismic catalogues

Prevalence of Aseismic Slip Linking Fluid Injection to Natural and Anthropogenic Seismic Swarms

An Atypical Shallow Mw 5.3, 2021 Earthquake in the Western Corinth Rift (Greece)

Fluid migration in low-permeability faults driven by decoupling of fault slip and opening

Transient evolution of permeability and friction in a slowly slipping fault activated by fluid pressurization

Migration of Fluid‐Induced Seismicity Reveals the Seismogenic State of Faults

Fault Trace Corrugation and Segmentation as a Measure of Fault Structural Maturity

Field-scale fault reactivation experiments by fluid injection highlight aseismic leakage in caprock analogs: Implications for CO2 sequestration

Collaborators (4)

Frantisek Gallovic

Frédéric Cappa

Philippe Charvis

Nicholas Voulgaris

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