Helmholtz-Zentrum Deutsches Geoforschungszentrum

Dipl.-Geophys. Maria Hurley

Funktion und Aufgaben:

Complex interdependencies exist between propagating dikes and topography. On one hand, topographic gradients have been shown to induce near-field stresses that control shallow dikes paths. On the other, dikes approaching the surface also lead to surface deformation: they may develop aligned eruption vents, associated subparallel fractures, and graben subsidence above the opening dike. These structures, still not fully understood, present complexities when occurring in non-flat areas.

My aim is to better understand this interplay. For that, I use satellite data and drone observations in real-case scenarios to conduct structural analyses and generate digital twin models. These are later used in simulations carried out in the analogue modeling laboratory. The study area of my Ph.D. is on Iceland, where exemplary cases exist (e.g., Laki), but also on La Palma, and elsewhere, allowing the development of unifying concepts to better understand how graben structures and volcanism interact worldwide.

Karriere:

PhD student, Thomas Walter and Fabio Bonalli as supervisors; Eleonora Rivalta as mentor.

Werdegang / Ausbildung:

2013-2019: Geology diploma at University of Buenos Aires. Thesis title: “Geology and structure of an Andean sector located between 36°10’ and 36°42’ S: Tectonic evolution of the northern Neuquen cordillera”.

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