Figure 1
From: Quaternary low-temperature serpentinization and carbonation in the New Caledonia ophiolite
Sample location. (a) New Caledonia position in the Pacific Ocean. (b) Simplified geological map of Grande Terre, featuring only the peridotite nappe and the regolith. (c) Simplified geological map of the southern part of the Massif du Sud with location of the studied samples (GR2H and Georges Pile) and hyper-alkaline springs (modified from Maurizot et al.30).
