FIELD TRIP


Natural Hydrogen System of the Pyrenees (SW France): a 2-days field trip

Serpentinization-sourced natural hydrogen is among the most well-studied generative systems worldwide. Its understanding has greatly benefited from observations of active systems at slow-spreading mid-ocean ridges, such as those located in the Atlantic. As oceans close to form mountain belts through tectonic cycles - a process known as the Wilson cycle -  these hydrogen-producing rock formations can be preserved and found within mountain belts, specifically in ophiolites—a term that encompasses rocks originating from ancient oceanic seafloors.
Over the past three decades, research has revealed that there are different ophiolites e going along with mantle rocks with distinct origins, compositions, geological histories and therefore hydrogen-generating potentials. This diversity is particularly striking in the Western Pyrenees, which has emerged as a hotspot for natural hydrogen exploration. In this area, mantle rocks of subcontinental origin were exhumed beneath sedimentary basins - such as the Mauléon basin - during a failed attempt to form an ocean ~100 My ago. Notably, the subsequent formation of the Pyrenees had a minimal impact on the pre-orogenic geology, preserving a high-potential mantle kitchen—a fault-controlled system connected to an upstream meteoric water recharge and a downstream hydrogen discharge area.

The aim of this field trip is to explore the key geological parameters of the Pyrenean system and its natural hydrogen system. On the first day, participants will follow the upstream plumbing system, tracing the path from the Pyrenean reliefs toward the mantle kitchen. The second day will focus on the mantle kitchen itself, extending to prospective exploration sites, with an emphasis on prospection technologies.

NOTES :
· Arriving place: Biarritz
. Date : November 11 & 12.
· Max number of participants: 20
Schedule:
  • 2 half-days in the field (can be flexible due to weather conditions in Nov)
  • 1 half-day in room (Geological introduction)
  • Printing: Field booklet
  • Material: need for good shoes and cold weather clothes.

In partnership with  : 

Natural Hydrogen System in the Lorraine basin (NE France) : a One day field trip

Natural hydrogen associated with the Carboniferous Sarre-Lorraine Basin in northeastern France represents a promising new frontier for hydrogen exploration. Unlike mantle systems, the hydrogen observed here is hypothesized to be generated by low-temperature water-rock interactions in deep sedimentary formations. Potential mechanisms include redox reactions with iron-bearing minerals in coal-bearing sequences and associated strata, or coal de-hydrogenation.


Recent advances from the REGALOR research program, utilizing innovative SysMoG™ probes, have identified significant concentrations of dissolved hydrogen in a historic water-saturated borehole located in Folschviller (Moselle, France). These findings suggest the existence of a deeper hydrogen source and the potential for an evolving accumulation of natural dissolved hydrogen in the aquifer. These results position the Grand Est region as one of the first in Europe to exhibit verifiable and quantifiable native hydrogen potential.


The objective of this field trip is to present the context of the Lorraine Carboniferous Basin, discuss the research and development processes that led to this discovery, and provide insights into new exploration engineering projects using dedicated wells. Participants will tour the Folschviller research platform and discover the facilities, focusing on subsurface monitoring tools and techniques. The second part of the trip will provide an overview of historical exploration efforts in the Lorraine Basin and future projects and operations currently planned in the region.

NOTES :
· Date : November 15 
· Max participants : 20






In partnership with :