Member Since 2016
Folarin Kolawole
Assistant Professor, Columbia University
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The Intraplate Stress Field of West Africa
GEOPHYSICAL RESEARCH LETTERS
04 june 2024
Jean-Joel Legre, Yan Qin, Folarin Kolawole, Tolulo...

West Africa continues to host a growing number of low and intermediate‐magnitude earthquakes (M2‐5) along its passive margins, and its ...

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Minimal Downward Saline Fluid Migration Near the Largest Injection-Induced Earthquake, Oklahoma
FAULT ZONE FLUID MIGRATION AND INDUCED SEISMICITY POTENTIAL IN GEOENERGY TECHNOLOGIES I POSTER
hydrology | 15 december 2023
Huy Le, Folarin Kolawole, Kerry Key, Micah Mayle, ...
The intriguing surge in widespread seismicity in the central and eastern US between 2009 2019 has been attributed to wastewater disposal associated w...
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Frictional behavior of hydrothermally-altered gouges: implications for fault stability of geothermal carbonate reservoirs
RUPTURE AND DEFORMATION PROCESSES, FROM SLOW TO FAST AND FROM MICRO TO MACRO III POSTER
mineral and rock physics | 15 december 2023
Jacob A. Tielke, Alessandro Verdecchia, Chelsea Pe...
Hydrothermally altered carbonate deposits are being targeted for geothermal reservoirs in much of Europe, and in particular in the Bavarian Molasse Ba...
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Interferometry of Ambient Seismic Noise Recorded by DRIAR Stations in the Northern Western Branch of the East African Rift System, Uganda
FROM CONTINENTAL RIFTS TO RIFTED MARGINS III POSTER
tectonophysics | 11 december 2023
Albert Kabanda, Ben Alonzo, Suzan van der Lee, D. ...
Ambient seismic noise interferometry is a method that harnesses noise into signals representing propagating surface waves, which we wish to utilize fo...
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Lateral Rift Propagation: A Top-Down or Bottom-Up Process?
FROM CONTINENTAL RIFTS TO RIFTED MARGINS I ORAL
tectonophysics | 11 december 2023
Folarin Kolawole, Rasheed Ajala, Jolante van Wijk
Continental rift systems grow by the lateral propagation, interaction, linkage, and coalescence of isolated rift segments. Prior to linkage and coales...
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Incipient Tectonic Reactivation of a ‘Failed’ Rift, Luama Basin, DRC
FROM CONTINENTAL RIFTS TO RIFTED MARGINS III POSTER
tectonophysics | 11 december 2023
Krista Watson, Folarin Kolawole
Continental rifts commonly undergo multiple cycles of failure and reactivation prior tobreakup. However, there remains limited understanding of the so...
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Evolution of Continental Rift Faulting: New Insights from the Incipient Okavango-Makgadikgadi Rift Zone, Botswana
FROM CONTINENTAL RIFTS TO RIFTED MARGINS III POSTER
tectonophysics | 11 december 2023
Cameron Grant, Folarin Kolawole, Jack N. Williams
Key questions remain on how fault scaling relationships evolve during the life of a continental rift from inception to break-up. We investigate the pa...
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Latest Advances of the DRIAR Project: Dry-Rifting In the Albertine-Rhino Graben, Uganda
FROM CONTINENTAL RIFTS TO RIFTED MARGINS III POSTER
tectonophysics | 11 december 2023
D. Sarah Stamps, Estella A. Atekwana, Eliot A. Ate...
Continental rifting is a critical component of the plate tectonics paradigm and is known to occur in more than one mode, phase, or stage. While contin...
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