- 1ITES, University of Strasbourg-CNRS, Strasbourg, France
- 2Mantle8, Grenoble, France
Native hydrogen (H₂) generated by the serpentinization of ultramafic rocks represents a promising clean energy resource, creating significant interest in the exploration of the Balkan ophiolite belts. However, the assessment and quantification of the H₂ potential are limited by the high variability and complexity of the Balkan ophiolites. Conflicting geodynamic models shifting between scenarios of isolated multiple basins and a single Neo-Tethyan ocean with hyperextended margins result in persistent uncertainties in the evaluation of the H2 potential. Since mantle fertility, fracturing, and hydration styles vary considerably among different scenarios, understanding the primary geodynamic context, i.e., the “tectonic kitchen”, is essential for predicting H₂ potential.
The aim of our study is to establish an integrated tectono-stratigraphic and petrological framework using the Vardar and Pindos ophiolite systems in Albania as key case study. A complete multi-criteria discrimination matrix was therefore developed, incorporating sedimentary budgets, basement architectures, magmatic systems and hydration types. This matrix allows for the distinction of ophiolitic environments by discriminating between Ocean-Continent Transitions (OCT), Mid-Ocean Ridges (MOR), Supra-Subduction Zones (SSZ), and Back-Arc Basins (BAB) using raw field data rather than pre-existing models.
These preliminary results help resolve local paleogeographic uncertainties and define the system’s initial conditions, setting the foundation for a thesis project dedicated to the characterization of mantle fertility, fracturing, and serpentinization dynamics. It will use these provenance data to decipher the variability of Tethyan ophiolites and thus establish a precise link between the characteristics of the mantle source rock, its geodynamic context allowing for the prediction and quantification of the potential for natural hydrogen.
How to cite: Blin, C., Ducoux, M., Masini, E., Domenighini, G., Mangenot, X., Ulrich, M., and Manatschal, G.: An integrated tectono-stratigraphic and petrological reassessment of the Vardar and Pindos ophiolite system and its significance for H2 exploration, 17th EGU Émile Argand Conference on Alpine Geological Studies, Fruška Gora, Serbia, 14–16 Sep 2026, alpshop2026-42, https://doi.org/10.5194/egusphere-alpshop2026-42, 2026.