Mineralogical and geochemical study of serpentinized peridotites from the North-Western Pyrenees: New insights on serpentinization along magma-poor continental passive margins

• Published in: Lithos 2021-12, Vol.406-407, p.106521, Article 106521
• Main Authors: Tichadou, C., Godard, M., Muñoz, M., Labaume, P., Vauchez, A., Gaucher, E.C., Calassou, S.
• Format: Article
• Language: English
• Subjects: Earth Sciences; Geochemistry; Hydrogen; Iron distribution; Mineralogy; Passive margin; Pyrenees; Sciences of the Universe; Serpentinization
• ISSN: 0024-4937; 1872-6143
• DOI: 10.1016/j.lithos.2021.106521

The peridotite massifs from the North-Western Pyrenean belt are fragments of a short-lived mid-Cretaceous hyper-extended rift inverted by the Pyrenean orogeny. We studied the petrology, mineralogy and geochemistry of 32 hydrothermally altered peridotites from the Montaut, Turon and Urdach massifs. This study aims to bring new constraints on the nature of serpentinization processes from domains having experienced various degrees of crustal hyper-extension and mantle exhumation in a context analogous to non-volcanic ocean-continent transitions. The three massifs studied are mainly composed of spinel-lherzolites and sample the same sub-continental mantle lithosphere as Eastern Pyrenean refertilized-peridotite massifs. They display contrasted degrees of hydrothermal alteration and serpentinization during cooling (e.g., serpentine contents ranging from 1 to 100 wt%) as well as variable reaction paths. The Montaut massif, located below an extremely thinned Paleozoic upper crust, records cooling from high temperature hydrothermalism with incipient serpentinization affecting mostly pyroxenes (serpentine, tremolite, talc, clinochlore assemblage; ~350–450 °C) to the formation of lizardite-chrysotile and magnetite after olivine (~200 °C–350 °C). The Turon peridotites, which remained below the detached Mesozoic pre-rift cover after complete removal of the crust, are little serpentinized and have no magnetite, suggesting serpentinization during the latest stages of cooling (< 200 °C). The Urdach massif comprises magnetite-bearing ophicalcites as well as magnetite-poor serpentinites formed concurrently when mantle was exhumed to the sub-seafloor at the margin toe (down to ~200 °C). Each massif shows selective enrichments in fluid mobile elements, in particular, Cs, Sb and Li, indicative of hydrothermal interactions with fluids deriving from neighboring sediments and continental crust, likely mixed with seawater-derived fluids for the Urdach peridotites. Our results show that the formation of magnetite in the studied samples is not tied solely to temperature, and point to a role of fluid composition in the development of the different serpentinization pathways observed from one massif to the other, and within a same massif in the case of Urdach. The development of complex sequences of temperature-, and composition-controlled reaction paths distinguish serpentinization in the Western Pyrenees peridotites from that commonly observed in the oceanic sub-seafloor. It results